Predatory scars in the shells of a Recent lingulid brachiopod: Paleontological and ecological implications MICHAŁ KOWALEWSKI, KARL W. FLEssA, andJONATHAN D. MARCOT Kowalewski, M., Flessa, K.W., & Marcot, J.D. 1997. Predatory scars in the shells of a Recent lingulid brachiopod: Paleontological and ecological implications. - Acta P alaeontologica P olonica 42, 4, 497-53f . The paper presents the detailed quantitative study of predatory scars in the shells of an inarticulate brachiopod: the lingulid Glottidia palmeri Dall, 1870. The scars include four morphological types: u-shaped,pocket, crack, and miscellaneous scars. They concentrate and open up toward the anterior shell edge. They commonly consist of a pair of scars on the opposite valves. The analysis of 820 specimens live-collected from two intertidal localities inthe northern Gulf of Californiaindicates that (1) 23. Vospecimens bearrepair scars; (2) the scars vary in size from 1.5 to 24 mrrt (mean = 2.5 mr#) and all scar types have similar size-frequency distributions; (3) the spatial distribution of scars on the shell is non-random; (4) the anterior-posteriordistribution of scars is strongly multimodal and suggests seasonal predation in the late fall and winter months; and (5) the frequency of scarred specimens increases with brachiopod size and differs between the two sampled localities, but does not vary among brachiopod patches from the same locality. The repair scars record unsuccessful attacks by epifaunal intertidal predators with a scissors-type weapon (birds or crabs). The high frequency of attacks, seasonal winter predation, and previous ecological research suggest that scars were made by winteńng shorebirds (willets or/and curlews). However, crabs cannot be entirely excluded as a possible predator. Because repair scars representunsuccessful predation, many of the quantitative interpretations are ambiguous. Nevertheless, the study suggests the existęnce of strong seasonal interactions between inarticulate brachiopods and their predators. Because shorebirds, crabs, and lingulids may have co-existed in intertidal ecosystems since the late Mesozoic, predatory scars in lingulid shells may have potentially a 100 million year long fossil record. Key predation, lingulids, brachiopods, Glottidia palmeri, shorebirds, words: Recent, B aja California. Michat Kow alew ski I michael.kowalew ski@ uni-tuebingen.de], Ins Ętut P aleobiolo gii PAN, ul. Twarda 5l/55, PL-00-8l8Warszawa, Poland. Karl W. Flessa [kflessa@geo.arizona.edu], Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA. Jonathan D. Marcot Idinosaur@ geo.ariTona.edu], Department of Geosciences, [.lniversity of Arizona, Tucson, AZ 85721, USA. 498 Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT Introduction Predatory attacksby durophagousorganisms(i.e.,those that damagethe prey's exoskeleton) create marks on the hard skeletons of their prey. In present-daybenthic marine ecosystemstraces of predationare very diverse (seeVermeij 1987 for details and references)and include drillholes made by snails, octopods,and flatworms (e.9., Bromley 1981; Kabat 1990; Kowalewski 1993); irregular punch holes made by stomatopodcrabs (e.g.,Geary et al. I99I); multĘle holes causedby fish (e.g.,Norton 1988);and fracture and breakageinflicted by crabs, birds, and other predators(e.g., Schoener1979;Vermeij 1987, 199f; Cadóe 1968, 1989;Vale & Rex 1988, 1989; Kropp 1992;Walker & Yamada 1993;Cadóe et al. in press). Predatory traces provide quantifiable data on prey-predator interactions, and thus,theyhavebeenintenselystudiedby biologistsinterestedin thebehaviorof prey and predators,foragingstrategies,populationbiology and ecosystemdynamics(e.9., Berg 1976;Wiltse 1980;Garrity & Levings 1981;Fairweather1985;Vale & Rex 1988, 1989).Moreover, predatorytracesare commonly preservedin the geological record. Indeed, they have a diverse and impressive fossil record and have been documented,in a greatvariety,from all the periodsof the Phanerozoic(e.g.,Vermeij 1987); and even from the Late Precambrian (Bengtson & Zhao 1992). Such fossilized traces of predation (Praedichnia;see Ekdale 1985; Bromley 1996) offer paleontologistsinvaluable insights into ancient ecosystems(e.g.,Hoffman et ąI. t974; Thomas t976; Robba & ostinelli 1975 Sheehan& Lesperancę1976;Kitchell et aI. 1981; Schindel et al. 1982;Hoffman & Martinell 1984; Kowalewski 1990; Andersen et al. 199|), into the bęhavior of extinct species (e.g.,Berg & Nishenko 1975;Kitchell 1986;Kelley 1989),and into macroevolutionaryand coevolutionary processes(e.g.,Vermeij1977,1987;Vermeijet al. 1980,1981,1982;Tayloret al. 1980;Ftirsich & Jablonski 1984;Allmon et al. 1990;Kelley 1989, 1991;Kelley & Hansen 1996). Here we presenta detailed quantitativeanalysis of the repair scars found on the shells of the Recent lingulid (family Lingulidae) brachiopod Glottidia palmeri Dall, 1870, a living fossil that inhabits the present-daymacrotidal flats of the northeastern Baja California, Mexico. In sharp contrast to repair scars in extant mollusks and articulatebrachiopods,which have been intenselyresearched(e.g.,Vale & Rex 1988, 1989;Thayer & Allmon l99I; Alexander 1992;Kropp 1992;Walker & Yamadal993; Walker & Voigt 1994;Cadóe et aI. inpress),repair scarsin extantlingulid brachiopods have not been investigated.In fact, ecological interactionsbetweenRecentinarticulate brachiopodsand their predatorshaverarely beeninvestigatedin a rigorousfashion (see James et aI. 1992;Emig in press;and below for references). This study has both biological and paleontologicalgoals. We documentthe morphological types of repair scars and attemptto identify the most likely predators.By doing so, not only do we hope to improve the ecological knowledge of present-day inarticulatebrachiopodsand their predators,but also to provide an actualisticdescription thatmay be helpful in identifying predatoryffacesencounteredin the fossil record of lingulid brachiopodsand othershelly organisms.Also, this studyillustratesdifficulties inherentto the interpretationof repair scars.Repair scars representunsuccessful predation events, and thus, provide ambiguous data on the ecology and behavior of ACTA PALAEONTOLOGTCA POLONTCA 42 (4) 499 prey-predatorinteractions,both Recent and fossil (see also Shoener 1979;Schindel et al. I98f; Vermeij 1983;Walker & Voigt 1994). We use repair scars to evaluate issues such as the size and site selectivity of predatoryattacks,variation in frequencyof predatoryattacksthroughtime and among different brachiopodpopulations,and seasonalityof predation.Our quantitativeanalysis servesalso to illustrate some statisticalmethodsuseful in analyzing repair sca.rs, both modernand fossil. In particular,we discussquantitativetechniquesthatallow for the assessmentof randomnessin the spatialdistributionof scarsand for therecognition of seasonalityof predationin modern and ancientecosystems. Previous research on durophagous predation on lingulid brachiopods In strikingcontrastto the Recentmollusks (e.g.,Vermeij1987,1992; Kabat 1990),the Recent lingulids has been poorly researchedfor tracesof predation.Marginal remarks and a few rigorous observationsscatteredin the literaturesuggestthatshells of the two Recent lingulid genera' Glottidią and Lingula, occassionally bear predatory marks. Drillholes has been relatively best documented.Paine (1963),in his monographon G. pyramidata, reportedthat drilled specimenswere commonly found (I4%oof shells containeddrillholes) on a sandbarnearthe mouthof Stum Pass (westcoastof Florida). A predatory drillhole, most likely caused by ą muricid gastropod' was found in G. palmerl (Kowalewski & Flessa 1994).Drillholes were also documentedin fossil lingulids from the Tertiaryof SeymourIslandSMiedmanet aL.1988;Bitner 1996)and the easternUSA (Cooper 1988).Among other inarticulatebrachiopods,predatory drillholes were reportedin Recent craniids (Emig in press) and in fossil acrotretids (Miller & Sundberg 1984;Chatterton& Whitehead 1987). Breakage and repair scars are poorly studiedin lingulids. The only more detailed observationwas reportedby Paine (1963) who investigatedholes made by willets (Catoptrophorussemipalmatus)and found many partially consumed specimens of G. pyramidata: 'In most instances,the pedicle and one valve were left, although in othersthe anteriorends of both valves had been broken off. If shell and otherdamage is not too extensive, the brachiopod can regenerateits lost portions' (Paine 1963: pp.I9f-193). Repair scars,most likely causedby crabs,were also found in shells of extantLingula (C.C.Emig writtencommunication1997).Breakageand repair scars, caused by durophagouspredators, Ta much better documented among articulate brachiopods,both Recent and fossil (e.9.,Brunton 1966; Thayer 1985;Alexander 1986a,1986b,1990,199f;Thayer& Allmon I99I; RuggieroI99I; Jameset al. 1992: Baliński 1993). To our knowledge, not only traces of predation but also predatorsthat prey on lingulids have rarely been investigatedrigorously.Nevertheless,previous researchers of lingulid brachiopods(e.g.,Paine 1963;Worecester1968;Emig et ąI. I978; Emig I98f ,1983)havelistedprosobranchgastropods,crabs,fish, andshorebirdsaspotential predators.In themost comprehensivereview so far,Emig (in press)provided a detailed list of predatorsincluding:(1) crustaceans(hermitcrabs,stonęcrabs,portunidcrabs, crangonids, stomatopods,shrimps, amphipods);(2) echinoderms (asteroids,op- 500 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT hiuroids, echinoids);(3) gastropods(muricidsand naticids);(4) fishes (demersalfishes and sturgeons);(5) shorebirds;and (6) humans. Gut contentstudiesprovide unquestionableevidencefor successfulpredation.The gutcontentof CatoptrophorussemipalmatusfromtheGulfof Mexico (Paine 1963)as well as the gut contentsof Limnodoromusgrieus,and C. semipalmatusfromthe Pacific coast of Costa Rica (Pereira 1990; Emig & Vargas 1990) indicate that those birds commonly prey on Glottidia. Also, the asteroid Amphipolis germinata frequently (437o) contains shells of Glottidia pyramidata (Emtg in press). Fish may also be importantpredatorsof lingulids. In the Gulf of Mexico, G. pyramidatą is preyedupon by estuarinesturgeons(Mason & Clugston 1993) and tonguefish(Cooper 1973).As reported by Campbell & Campbell (manuscript),one specimen of sturgeonin the Florida Museum collections contained 500 specimens of G. pyramidata. Lingula anatina was commonly found in the stomachsof demersalfishes (Emig in press). In sum, this brief review indicates that, in present-dayecosystems,a variety of predatorsprey upon lingulid brachiopodsand can potentiallyleave predatorytraceson shells of their victims. Material and methods Study Area. - The study area is the intertidal mudflat of the southernmostdelta plain of the Colorado River, north of San Felipe, Baja California, Mexico (Fig. 1).The tidal flat experiencesextremelyhigh semi-diurnaltides with tidal rangesreachingup to 10 meters(Sykes 1937 Roden 1964;Thompson 1968;Bray & Robles 1991).The intertidalflat reachesup to severalkilometersin width. This exceptionalmacrointertidal environmentis inhabitedby an abundantmacroinvertebratefauna (seeThompson 1968; Batten et ąl. 1994) that includes the infaunal lingulid brachiopod Glottidia palmeri Dall, 1870(Dall 1920;Thompson1968;Kowalewski 1996a).The climateof the area is hot and arid with a maximum summer temperatureof 50'C and less than 60 mm precipitationper year (Ezcurra & Rodrigues 1986;Thomson 1993).The water of the northern Gulf of California has a salinity of 3G39%o (Brusca 1980). Mean monthly watertemperaturereachesabout30"C in the summerand drops to 15'C in the winter (Thomson 1993). The tidal flat is a progradationalfeaturecomposedof fine-grainedclastic sediments consisting predominatelyof silts and fine-grainędsands.Several seńes of longitudinally oriented,shell-rich beachridges occur in the area(Thompson1968;Kowalewski et aI. 1994).The facies developmentof the tidal flat, discussedin detail by Thompson (1968), has largely been controlled by the activity of the Colorado River (see also Kowalewskj et ąl. 1994;Kowalewski & Flessa 1995). On Glnttidia palmeri Dall, 1870.- This species is endemic to the Gulf of CaliforniaandthePacificcoastofCalifornia(Datl1870,l87t,l9f0:Lowe l933;Hertlein & GrantL944;Thompson1968;Emig 1983;Kowalewski1996a).Itwasdescribedfirst by Dall (1870)from the intertidalmudflatsof northeasternBaja California, where it is patchilydistributed,but locally very abundant(Thompson1968;Kowalewski 1996a). Like all other Recent lingulids (e.9.,Paine 1963; Emig et al. 1978; E-ig 1982; ACTA PALAEONTOLOGTCA POLONTCA 42 (4) 501 Fig. 1. Map of the study area showing the location of the two sampling localities. A. Regional map (Baja California and the Gulf of California). B. The northernGulf of California and the Colorado River Delta (Fig. 1B modified from Thompson 1968;Kowalewski et al. 1994). Treuman& Wong 1987),it is an infaunal suspension-feederthat lives in deepvertical burrows and is anchoredby a long pedicle (seealso Kowalewski & Demko 1996).Its shell is thin (0.2--0.3mm), spatulate,and linguliform in outline, and reaches up to 45 mm in length. The shell has low internal septa- a diagnostic featureof the genus Glottidią (Rowell 1965; Emig 1983).The ventral,or pedicle, valve has two septa diverging from the beak. The dorsal, or brachial, valve has one median septumand is slightly shorterthan its ventral counterpart.The shell consists of calcium phosphate and containsas much as 50Voorganicmatter(G. Goodfriendpersonalcommunication). Shells display yellow or occasionally greenor dark brown color banding. Concentric growth lines are often visible. Previous work on G. palmert concentratedprimarily on its taxonomyand morphology (e.g.,Dall 1920;Hatai 1938;Hertlein & Grant 1944;Emig 1983).Arecent study by Kowalewski (I996a) indicated thatG. palmeri occurs in denselyinhabitedpatches dominatędby single age-cohorts(see below for more details).Little is known about causes of mortality in G. palmeri. Predation and seasonalmortality during winter 502 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT months- when stormserodeand redepositintertidalsedimentsor when watertemperaturesdrop beyondthe brachiopod'stolerance- are most likely factors (Kowalewski & Flessa 1994;Kowalewski 1996a). Field,laboratory and analytical method Ttris analysis is basedon the SźImples collectedby our researchgroup to investigatethe taphonomy,populationbiology, biometry,and naturalhistory of G. palmeri (seeKowalewski & Flessa 1994;Batten & Kowalewski 1995;Smith et al. 1995;Kowalewski 1996a;Kowalewski e/ al. 1997; Anand et al. submitted).The samples were collected from two localities on the macrotidalflat of the lower Colorado Delta (Fig. 1). Six patchesfrom thetwo localities (Fig. 1)were sampledin March L993,Novęmber 1993,and February 7994.This analysis includes the live-collected specimens,which were previously measured(Kowalewski I996a),but not analyzedfor scars (n = 599), as well as additional live-collected specimens not included in the previous study (n - ZfI). All additional specimenswere measuredto the nearest0.1 mm using electronic or dial calipers. Size of the shell was measuredas the length of the longer, ventral valve. This procedureis consistentwith the one employed previously (Kowalewski 1996a). The population data,basedon 820 specimens,are summarizedin Tablę 1. Pręvious quantitativeanalysis (Kowalewski I996a) indicated that patchesfrom Locality One representedsingle age-cohortsfrom single spatfalls and consisted of mature,slowly growing specimens that were 34 years old at the time of collection. The new population data,with an increasedsample size (numberof specimens),are consistent with the previous work. Note that the mean specimensize in Locality One increased by f .4 mm from March 1993 to November 1993, but did not increase in size form November 1993 to February 1994 (Table 1). This is consistent with growth ring analyses(Batten& Kowalewski 1995;Anand et al. submitted)which indicatesthatG. palmeri ceasesor slows its growth during winter months.Locality Two, in the north, includedyoungerpatchesof variousage,representingI2 yearold cohorts(Table1). Table 1. Size datafor the Glottidia palmeri patchessampledin March 1993,November 1993,and February 1994.This analysis,basedon 820 specimens,updatesthe previous analysis,based on 599 specimens(see Kowalewski I996a: table 1). Variable March 1993 November 1993 February1994 154 36.8 3f5 39.2 1.86 44.8 33.s r72 39.1 1.53 45.8 35.4 45 28.2 4.58 36.3 fr.6 rf4 24.7 2.00 f8.4 19.1 Locality One Sample size Mean (mm) Standard deviation (mm) Maximum size (mm) Minimum size (mm) r.4z 39.s 32.f Locality Two Sample size Mean (mm) Standard deviation (mm) Maximum size (mm) Minimum size (mm) ACTA PALAEONTOLOGTCA POLONTCA 42 (4) s03 Each specimenwas carefully examinedunder magnificationfor any marks (scars, cracks, growth disruptions,etc.). Marks were classified according to their presumed ońgin as: (1) reliable marks that were, in our opinion, predatory in origin; and (2) questionablemarks which were fresh-looking,unnaturally straight,much larger than otherscars,and cut randomly acrossthe shells at various angles(mostlikely thesewere caused by our shovels when we were digging for specimens or during subsequent transport_ see also Flessa et ąI. 1992).We confined our analysis primarily to the reliable scars. The size and location of each scar was measuredusing a ffansparentgrid. A sector in the grid covered approximately 3 mmz. The scar size was estimatedvisually by comparing the area covered by the scar to the grid. For example,the size of the scar that covered areacoffespondingto 1.5 sectorwas recordedas 4.5 Ń. The precision of the estimatewas ł1.5 mmz (i.e.,t0.5 sector).To estimatethe positionof the scar, the grid was placed over each specimenwith the lateral sector '1' placed at the anterior shelledge(Fig. 2A). Note thatscarlocationcanbe describedconsistentlyusinga single grid systemonly for specimensthat are similar in size and were collected at the same time (theapparentposition of scars in relation to the grid 'shifts' with shell growth). To estimatethe relative age of the scar,we measured,to the nearest0.1 mm, the distance (Ą from the youngest shell growth ring disrupted by the scar to the anterior (growing) edge of the shell. Assuming that scars were made at the growing edge of the shell, d canbe used to estimatethe relative ageof the scar' ŹNwell as to calculatethe size of the brachiopodat the time of affack (S') (seeFig. 2B). The assumptionthat scars were madeat theanteriorshellmarginseemsreasonablein view of Paine's (1963)observations on predatorydamagetnG. pyramidata(seeabovefor details).Nevertheless,we will note some alternativeinterpretationsfor our data,when this assumptionis relaxed. Note that both, d and,Sa,estimatethe relative age of the scar (Fig. 2B). However, dis a more appropriatemeasurebecause itminimizes thenoiseinffoducedbyvariationinbrachiopod growthrate:modernlingulids show an asymptoticgrowthrate(e.g.,Chuang l96l;Paine 1963;Worcester1969;Kenchington& Hammond 1978),and thus,the variationinfroduced by differencesin the growth rate among specimensshould substantiallydecrease towardthe anteriorshell edge.In the caseof complementary(paired)scars,the distance was measuredfor the scar closer to the anteriorshell margin. Note that the distance analysis is appropriateonly for Locality One, because all specimens in that locality belong to the same agelsize cohort (i.e., d is directly comparableamong the specimens).Because the brachiopodpopulationgrew f .4 mm betweenMarch 1993 and November 1993 (see above and Table 1), we conected d values for shell growth for the March 1993 sample (i.e., d - d + 2.4). Because the specimensdid not grow significantly betweenNovember 1993andFebruary 1994,the November samples were not corrected.After the correction is applied, all distance measurementscan be treatedas if they were taken at thę Samętime in February |994. The morphology of each scar was describedand a schematicdrawing of the scars outline was made. Most of the scars could be classified into three morphological categorieshereafterreferredto as: 'u-shapedscars', 'pocket scars', and 'crack scars' (see Fig. 3), scars with other morphologieswere classified as 'miscellaneous'.The scars were also classified as either healed (complete repair of all shell layers) or unhealed (incompleterepair with external shell layers still disrupted).A substantial 504 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT A Anteriorshelledge \ ź \ tĘ 95 o o oo a c Ń8 .E o E9 Sa, Sa, 10 11 12 13 't4 15 16 't7 I \ \ \ / f / -3-2-1123 Verticalsectors Posteriorshellend , 5 mm , Fig. f , A. Grid systememployed in this study to estimatethe position of a scar on the brachiopod shell in plan view. A hypotheticalscar is locatedin sector- 1,3. one sectorof a gńd representsa square=3 mmz in area. B. Schematic illustating the measurementmethod used to estimated the relative age of the scar and thebrachiopodsize at the time of theattack.Two hypotheticalscarsare usedas examples.Scar 2 is younger thanScar 1 (i.e.,dt > dz) and was inflicted on a largerspecimen(Sat < Saz). Symbols:dt - distanceof Scar 1 from the anterior shell edge, dz - dtstanceof Scar 2 from the anterior shell edge, Sat - the size of the brachiopod at the time of attack recordedby Scar 1, Saz _ the size of thę brachiopodat the time of attack recordedby Scar 2, L - the anterior-posteriorlength of the shell. proportionof the scarsconsistedof two complementarydisruptionson oppositevalves. Such paired scarsweretreatedin our analysisas single observationsandmeasurements were taken only for one of the two disruptions;whichever was more appropriatefor a given measurement(seethe example of distancemeasurementabove). All statisticalanalysis were performedusing StatisticalAnalysis System (SAS) on the University of Arizona interactive VAX system. The statistical analyses were performed using the SAS/STAT procedures(SAS Institute 1989, 1990a).Statistical randomizations and simulations were written in the SAS and SAS-IML languages (sAs Institute1990a,1990b,1991). ACTA PALAEONTOLOGTCA POLONTCA 42 (4) 505 Results containedat Out of 820 live-collectedspecimensof Glottidia palmeri,267 (32.6%o) leastone disruption(Thble2). Among them,75 specimens(9.|Voof all specimens)bear 'questionabledisruptions'.Thus, we classified only f3.47o of collected specimens (n = 192) as having 'scars' of unquestionablybiogenic origin. The quantitativeanalysis, presentedbelow deals primarily with the unquestionablescars. Because some specimensbear multiple scars,the total numberof scarsexceedsthe total numberof specimens(Table2). For example,thereare2I3 unquestionablescars, but only 192 specimensthatbear them.Similarly, 75 specimensbearonly questionable disruptions,but thereis a total of 85 questionabledisruptions.Thus, the sample sizes and results vary dependingon the objective of analysis. Note that it is importantto distinguish betweenthe analysis that targetsscars and the analysis that targetsspecimens. In general,the analysis of scars provides information about the predatorand analysesof specimensprovides information aboutthe prey. For example,65 (33.9Vo) specimensbear healed scarsbut there are total of 70 (32.97o)healed scars.Obviously, 33.97oof the attackedbrachiopodsweręable to heal their shells completelyby thetime of collection,and not 3f.9Vo.Similarly, we identifiedtotal of 84 u-shapedscarsbut there are only 78 specimens bearing them. When studying the site-selectivity of predation,one should analyze all 84 scars, even thoughthere are only 78 specimens that contain them. We explicitly distinguish between the two types of analysis by presentingthem in the two separatesęctions.Although this distinction may appearto be trivial, not distinguishing between 'traces' and 'specimens with traces' would seriously underminethe clarity of any quantitativeanalysis. TYpes of scars. - Although scars vary in shape,most of them can be categorized into one of the three main morphological types (Fig. 3) referredto here as 'u-shaped scars', 'pocket scars', ffid'crack scars'. The remainingscars (17.8%o) could not be assignedto any of these morphological types and were classified into the 'miscellaneous'category. Ninety disruptionswere identified as u-shapeddisruptions.Only six of them were questionabledisruptionsand 84 were identified as true scars (39.4Voof all scars).The scars have a regular u-shapedoutline (Fig. 3,Ą) with their two arms typically open directly toward the anterioredge of the shell (i.e.,the scar axis is parallel to the shell axis). The ratio betweenthe length of the arms and the width of the 'u' ranges from 2:1 to 3:1.In many cases,u-shapedscarsconsistof two complementarydisruptionsof similar size located on the oppositevalves and situatedat a similar distancefrom the anterioredge of the shell. Fifty seven disruptionswere identified as pocket disruptions.Only seven of them were questionabledisruptionsand 50 were identified as ffue scars (23.5%o of all scars). Pocket scars (Fig. 3B) have a much more complicatedoutline than u-shapedscarsand can be describedas deeppocketsthatform irregulardisruptionsin the shell. They also open toward the anteriorbut they are much more elongatedthan u-shapedscars with theratio betweenthelengthof the arms andthe width of the scarrangingtypically from 5:1 to 10:1.Unlike the u-shapedscars,the majorityof the pocketscarshave their axis at an acute angle (10-20') to the shell axis. In many cases,the pocket scars consist of 506 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT Tablef . Summary of quantitativedata on predatoryscarsin shells of Glottidiapalmeri. Variable Total number Locality One percent number percent Locality Two number percent 100.0 61.0 39.0 28.1 10.9 4.0 2.4 0.3 0.3 169 r56 9 I 0 2 64 66 83 34 100.0 8.1 1.1 4r.5 f3.0 18.0 r7.5 65.0 35.0 36.r 45.4 18.6 100.0 28.5 7r.5 284 81 203 100.0 28.5 7r.5 t4 f13 r43 70 84 50 4l 38 81 94 38 100.0 67.1 3f .9 39.4 f3.5 19.f 17.8 38.0 44.r r7.8 f03 134 69 82 46 39 36 78 89 36 100.0 66.0 34.0 40.4 ff.7 19.f 1'7.8 38.4 43.8 r7.8 l0 9 I 2 4 f 2 5 f 100.0 90.0 10.0 f0.0 40.0 f0.0 f0.0 30.0 s0.0 50.0 U-shaped disruptions questionable disruptions scars 90 6 84 100.0 7.1 92.9 88 6 82 100.0 6.8 93.f f 0 f 100.0 0.0 100.0 Pocket disruptions questionabledisruptions 57 7 50 100.0 r f. 3 8'7.7 53 7 46 100.0 13.f 86.8 4 0 4 r00.0 0.0 100.0 8f 4I 4l 100.0 50.0 50.0 78 39 39 100.0 50.0 s0.0 4 2 100.0 50.0 50.0 69 100.0 44.9 55.1 65 29 36 100.0 44.6 55.4 Specimens without any disruptions with disruptions with scars with questionabledisruptions withf disruptions with 2 scars with 3 disruptions with 3 scars 820 553 f67 r9f 15 27 I7 2 2 100.0 67.4 3f .6 Specimens with scars with 2 scars with 3 scars with u-shaped scars with pocket scars with crack scars with miscallaneous scars with healed scars with unhealed scars with a scar on a ventral valve with a scar on a dorsal valve with a paired scar on both valve r92 77 183 I6 2 76 4f 65 rf1 68 88 36 r00.0 8.8 1.0 40.6 23.4 18.2 r1.7 33.9 66.r 35.4 45.8 18.8 Disruptions questionable disruptions scars f98 85 213 Scars unhealed scars healed scars u-shapedscars pocket scars crack scars miscellaneous scars scars on ventral valve scars on dorsal valves paired scars on both valves SCATS Crack disruptions questionabledisruptions SCATS Miscellaneous disruptions questionable disruptions SCATS L 78 45 35 3+ a 1 J I 38 23.+ 9.r J.J f.r 0.f 0.f 651 391 254 183 71 f6 16 a L z JJ JL n9 1 a IJ 9 4 I 1 0 0 100.0 92.3 1.1 5.3 L.A 0.6 0.6 0.0 0.0 100.0 11.1 0.0 ff.f J JJ.J f 22.2 L 8 1 L 5 f + l0 J Z L f zz.f 88.9 11.1 22.2 55.6 22.2 r00.0 28.6 1r.4 100.0 50.0 50.0 ACTA PALAEONTOLOGICA POLONICA 42 G\ 507 Fig. 3. The threemain morphological types of scars (anowed) identified in shells of the inarticulate lingulid brachiopod Glottidia palmeri, Locality One. Detailed descriptionsare provided in the text. A. U-shaped scar.B. Pocket scar.C. Crack scar.All specimens reposited with the lingulid brachiopod collection of the InvertebratePaleontologyLaboratory (Departmentof Geosciences'UniversĘ of Arizona,Tucson,USA). two complementaryscars of similar size located on opposite valves and situatedat a similar distancefrom the anterioredge of the shell. Thanks to all thosedifferences, and the factthat very few scars displayed intermediatemorphological characteristics, the pocket scars were easy to distinguishfrom the u-shapedscars in our samples. Eighty two disruptions were identified as crack disruptions. Half of them were questionabledisruptionsand only 41 were identified as true scars(I9.27oof all scars). Crack scars are linear disruptions(Fig. 3C). In many cases,the scars consist of a pair of cracks that form a v-shapeddisruption which invańably openstoward thę anterior edge of the shell (Fig. 3C). In many cases,the cracks consist of two complementary scars of similar size located on the oppositevalves and situatedat a similar distance from thę anterioredge of the shell. Sixty nine disruptions could not be classified in any of the three morphological categoriesand were,therefore,classified as 'miscellaneous'.Almost half of them were questionabledisruptions,and only 38 wereclassifiedas truescars(I7 .8%o of all scars). Some of the miscellaneousscars also open toward the anteńor edge of the shell. ln 508 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT 140 120 n -203 tTt- 2.5 S=2.3 I(s 1 0 0 o u)80 o b60 -o E40 L E =t z 5 zio 20 0 fi=82 rfi= 2.1 S= 1.1 a b40 o u, b30 o -o 20 1 1.5 2 2.5 3 1.5 2 3.5 4 4.5 Scar size (mm') Ę20 (u o fi=46 tTt= 2.5 S= 1.5 O o15 o -o E10 L 2.5 3 3.5 4 Scar size (mm') I 830 fl=39 t T= I 1.7 S=0.8 a b25 bzo -o Ę15 z10 z J 5 0.5 1 1.5 2 2.5 3 3.5 4 4.5 Scar size (mm') 0.5 1 1.5 2 2.5 3 3.5 4 4.5 Scar size (mm') Fig. 4. A-D. Size-frequencydistribution of scars from Locality One. A. Pooled data for all scar types. B. U-shaped scars. C. Pocket scars. D. Crack scars. Symbols: n - sample size, m - mean, s - standard deviation. many cases, the scars consist of two complementary scars of similar size located on the opposite valves and situated at a similar distance from the anterior edge of the shell. Quantitative analysis of scars. - The overwhel-ing majority of disruptions (95.3Vo)were found in specimens collected from Locality One. The quantitative analysis can, therefore,be confined to Locality One without substantiallyreducing sample sizes (see Table 2). This allows us to eliminate any potential uncontrollable variationin the datacausedby biotic and/orenvironmentaldifferencesbetweenthetwo localities. The analysis was performedboth for all scar types pooled together,as well as, separatelyfor each of the threemorphological types of scars (miscellaneousscars were not analyzed separately). The size of scarsvariesfrom 1.5mmz to 24 ffi and averages 2.5 Ń (Fig. aA). The variation in scar size is relatively small, with standarddeviation of 2.3 mmz and coefficient of variation, cv = 9tVo. The size-frequencydistribution is highly rightskewed(skewness= 5.4) and very peaked(kurtosis= 41.8)with themajorityof scars ACTA PALAEONTOLOGTCA POLONTCA 42 (4) 509 r= 0.32 P =0.0035 tl=82 (u-shapedscarsonly) aoaa aa Oa (f 0510152025 30 35 40 45 50 Brachiopodsize at thetimeof theattack[Sa](mm) Fig. 5. Scatter plot of ,Sa(size of the brachiopod at the time of the attack) vs. scar size. Data for u-shaped scars from Locality One (the other two scar types do not show any significant correlation).Symbols: r Spearmanrank correlationcoefficient,p - significance of the correlationcoefficient,n - sample size. being small. The analysis by scar type reveals a very similar patternin all threecases. All distributionsare strongly right-skewed,vary in a similar size range (Fig. 4B-D), and are statisticallyindistinguishablefrom one anotherin their overall shape(pairwise Kolmogorov-Smirnovtest,p > 0.05 in all threecases).Moreover,the u-shapedscars and the pocket scars do not differ significantly from one anotherin their median size (Wilcoxon test,p = 0.06).The only exceptionis the significantly smaller size of crack scars in comparison with the two other scar types (Wilcoxon test,p <<0.05 in both cases). Howeveą given that the scar size, as defined here, is an area measure,the relatively smaller size of the crack scars should not be surprising. As explained above,the distanceof the scar to the anteriorshell edge can be used to calculate the brachiopod size at the time of the attack (So)(seeFig. 2B). Spearman rank correlationanalysis indicatesthat only in the case of the u-shapedscars,does the scar size (S) and the brachiopod size at the time of the attack (So)show a significant positive correlation(p = 0.0035,Fig. 5). However, althoughsignificant,the correlation is not very strong(Spearmanrank coefficient,r = 0.32,Fig. 5). Out of 203 scarsfrom Locality One, I7 .87oof the scars occurredon both valves of the brachiopod(i.e.,scars were representedby a pair of disruptions).Out of 167single scars, 46.7Vowere located on ventral valves and 53.3Voon dorsal valves. This proportion does not differ significantly from 50:50, p - 0.28 (binomial test with normal approximation,seeZar 1984).The dorso-ventraldistributionof scars is very uniform among the three scar types: in all cases, the paired scars representless than 207o (Fig. 6). The proportion of single scars on dorsal vs. ventral valves does not differ significantly from 50:50 (in all three casesp >>0.05, binomial test).Also, the homo- Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT 510 G =5.05 P = 0.282 n=167 E60 o g o tL ło Proponion of scars | located on dorsal valves tilllllTl Prooortionof scars ]łi:ii:ii:l |ocdtedon ventra|va|ves l-l | A' tuo3l",. #:' rYPe 3 ! I Proportionof paired scars located on both valves Fig. 6. Dorso-ventral distribution of scars shown for the pooled data and separatelyfor each of the three main scar types.Data for Locality One only. The numbersabove each bar representthe sample size of that bar. Symbols: G - log-likelihood ratio (G-statistic),p - significance of G, df - number of degrees of freedom,n - sample size. geneity G-test (Fig. 6) fails to indicate any statistically significant variation in dorsoventral distributionof scars among differentscar types. Analysis of the spatial distribution of scars in the plan view was limited to November 93 and February 94 samples from Locality One. We excluded the March 1993samplebecause,due to the shells' growth,the apparentposition of scars oshifted', on averageby2.4 mm (seeabove).Thus, we analyzedtotal of 182 scars.For all three scar types, the spatial distribution of scars appears highly non-random with the majority of scars located in the anteriorpart of the shell and concentratedalong the shell's median axis (Fig. 7A-C). Note that even though there are potentially 17 horizontal sectors(seeFig. 2A), only sectors1 through If contńn scars.The only obvious differenceamongthethreescartypesis in their distributionparallel to the anteriorshell edge (i.e., along lateral sectors).U-shaped scars concentratealong the median shell axis, whereaspocket scars and crack scars are more evenly distributed and include many scars located along the lateral margins. The apparentnon-randomnessin scardistribution(Fig. 7) canbe analyzedrigorously using a Poisson model. In this paper,we proposean approachwhich uses a Monte Carlo simulationbasedon the Poisson probability function (for detailsseeAppendix 1; see also Reyment l97t). The simulationsindicate that the spatial distributionof scars is significantly differentfrom random for each of the threescar types,p < 0.0001 (the sameresult is obtainedfor the pooled data). Out of 203 scarsfrom Locality One, only 33Voarecompletelyhealed(Fig. 8).Therb is a statistically significant variation in the proportion of healed scars among the differentscar types (see Fig. 8). U-shaped scars show the highestrate (over 52Vo), whereas only =25Eoof crack and=l3Vo of pocket scars are healed.Healed scars and unhealed scźLrs differ dramatically in their distribution away from the anterior shell edge. The mean distance d is 5.9 mm (median = 3.3 mm) for unhealed scars, and ACTA PALAEONTOLOGICA POLONICA 42 (4) 511 10 8 6 4 2 NUMBER OF SHELLS 0 ^ł'il s6crob 1'x._ NUMBER 12 OF SHELLS 10 12 10 I 6 4 2 0 8 6 4 2 0 6 3 4 3 2 NUMBER 6 oF st-{ELLS 5 1 0 4 3 2 1 0 Fig. 7. Spatial distribution of scars on brachiopod shells in plan vięw. Data for the November 1993 and February 1994 samplesfrom Locality One only. Note thatlateralsector '1' correspondsto the anteriorshell edge (to relate the charts to the brachiopod shell see also Fig. 2A). Symbols: p - probability that spatial distribution of scars is random (basedon Monte Carlo simulations,see text and Appendix 1), n - sample size.A. U-shapedscars.B. Pocket scars.C. Crack scars. 13.8mm (median= 16.1 mm) for healed scars.This differenceis highly significant statistically(p <<0.05,Wilcoxon test).The increasein the proportionof healedscars away from the anterior shell edge is not surprising consideringthe fact that the more posteriorscars are older, and thus, more time was available for their healing. 512 Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT G = 23.4 P = 0.001 n=167 E60 o I o (L40 20 1-1 Proportion | | of unhealed scars 163 Proportion li:i:i::ii::l of healed scars 0 All Type 1 Type? Scar type Type 3 Fig. 8. The proportionofhealed to unhealędscars shown for the pooled data and separatelyfor each of the threemain scar Ępes. Data for LocaliĘ one only. The numbersabove each bar representthe sample size of thatbar.Symbols: G - log-likelihood ratio (G-statistic),p - significanceof G, d.f- numberof degreesof freedom,n - sample size. $H go $ E =.-i.- F0.036 F0.005 t ^ E i F0.065 c.. o) o) o '= e.0.402 = 25 (U o a o20 o L € =1s z 0 1 2 3 4 5 6 7I91011 1 2 1 3 1 41 5 1 6 1 7 1 81 9 2 0 2 12 2 2 9 2 4 2 5 2 6 2 7 2 8 2 9 3 0 3 1 Distancefromthe anteriorshell edge (mm) Fig. 9. The anterior-posteriordistribution of scars on the brachiopod shell (i.e., distance-frequency distribution).Data for Locality One only. Four major modes may represenrseasonal(winter) predation. Note the increasein spacingbetweenthe modes away from the anteriorshell edge.The two anteriormodes are statisticallysignificantaccordingto 10,000-iterationbootstrap(seeAppendix 2). Symbol:p - bootstrap estimateof local sisńficance of a mode. ACTA PALAEONTOLOGTCA POLONTCA 4f (4) 513 Scartype: miscellaneous 925 (U o a o20 o -o crack scars pocket scars u-shaped scars =1s z 01 23 4 5 6 7I910 1 1 1 2 1 3 1 4 1 51 6 1 7 1 8 1 9 2 0 2 12 2 2 3 2 4 2 5 2 6 2 7 2 8 2 9 3 0 3 1 Distancefromtheanteriorshelledge(mm) Fig. 10. The anteńor-posteriordistribution of scars on the brachiopod shell (i.e., distance-frequency distribution).Data the sameas for Fig. 9, re-plottedhere to show the variation amongthe scar types in their anterior-posteriordistńbution. Scars vary in their distanceto the anteriorshell edgefrom 0 to 31 mm. This means, given the average size of specimens(see Table 1), that scars are absentin the most posteriorpart of the shell (6-9 mm; seealso Fig. 7). The distributionof scarsaway from the anterior shell edge is strikingly multimodal (Fig. 9), with four well defined modes. The first mode is locatedat the anteriorshell edge (0-1 mm distanceclass),the second and largest mode is located 3 mm toward the posteńor from the first mode (3-4 mm distanceclass).In addition,therearetwo smallermodestowardtheposteriorof the shell: 8-9 mm and 17-18 mm distanceclassesrespectively.Note thatthe spacingof the modes increasesaway from the anteńor edge (Ftg. 9). We used a bootstrapprocedureto test whetherthe modes are statistically significant (for details seeAppendix 2). The analysis suggeststhat two anteriormodes are statisticallysignificant,whereasthe two smaller posterior modes are not (see Fig. 9). The two posterior modes became significant, however,whęnchartresolutionis decreasedto 2-mmbins (notshownhere). The three main scar types differ notably in their anterior-posteriordistribution (Fig. 10). Crack scars and pocket scars concentratemostly in the anteriorpart of the shell (0-11 mm distanceclasses),whereasu-shapedscars dominatefartheraway from theanterioredge(12-31 mm distanceclasses).Given thatthefrequencyof healedscars increasesaway from the anterioredge,themoreposteriordistributionof u-shapedscars is consistentwith their significantly higher frequencyof healing (Fig. 8). The u-shaped scars differ statisticallyin their anterior-posteriordistributionfrom the two other scar types (in both comparisonsp<<0.05,pairwiseKolmogorov-Smirnovtest). Quantitative analysis of brachiopod shells. - Out of 820 brachiopodspecimens, 23.4%o bear repair scars (seeTable Zfor quantitativesummary).Out of 192 specimens 514 Predatorvscars: KOWALEWSKI. FLESSA. & MARCOT r= O.75 P =0.0003 8so fi=18 I(u o g40 o C) 5 =s o o E o20 (s &10 15 Shell length(mm) Fig. 11. Scatter diagram showing frequency of scars in a given size-class of brachiopodsplotted against brachiopod size-classes.Only the size-classeswith n > 5 arc considered.Data pooled for Localities One and Two. Symbols: r- Spearmanrankcorrelationcoefficient,p - significanceof the correlationcoefficient, n - sample size. with unquestionablescars, 9O.2Vospecimensbear single scars, 8.8Vobear two scars, and only 2 (IVo)bear three scars. Specimensbearing more than three scars were not identified among our samplęs. The frequencyof attackedspecimensincreaseswith brachiopodsize: whereasshells with scarsare rare in the smaller size classes,they becameincreasinglyfrequentamong largerspecimens.lndeed,thereis a very strongpositive correlationbetweenthefrequency of attackedspecimensand their size (Fig. 11).Also, the frequencyof specimenswith multiple Scars increases with the brachiopod size. The mean shell sŁe of specimens bearing multiple scarsis significantly greaterthanthemean size of specimenswith single scars(Z = 2.51,p =0 .Ul2,Wilcoxon test).The specimenswith multiplescarsareconfined to larger brachiopodsize-classes.Smallest specimenwith multĘle scals has length of 35.6 mm, whereasspecimensas small as20 mm containsingle scars. The frequencyof attackędindividuals of G. palmeri varies at thethreecomparative levels that are available given our sampling design: (1) betweenlocalities; (2) within Locality One amongbrachiopodpatches;and (3) within Locality One throughtime. 1. Variation between the two localities. The most dramatic variation can be observedbetweenthetwo sampledlocalities(Fig.tf; Table2). Specimenswith scarsare over threetimes more frequentin Locality One thanin Locality Two. In both localities, the frequencyof attackedspecimensincreasesin thelargersize-classes.However,only in thęcaseof Locality one is this patternstatisticallysignificant(seeFig. 12).The lack of significancefor datafrom Locality Two may be a consequenceof the smaller sample size (only 9 specimenswith scars). 2. Yariation within Locality One. Because three patchesfrom Locality One were sampledsimultaneouslyin November 1993,it is possible to analyzelocal (within-lo- ACTA PALAEONTOLOGTCA POLONICA 4f (4) 515 tlt= 468,Dz=183 M , = 3 8 . 4 ,M z = 3 8 . 9 Z = 3 . 3 9 ,p ( Z ) = 0 . 0 0 0 7 D = 0.144,p(D)= 0.008 (/, 100 o -c U' b80 o -o L Ę60 z tl.,= 1 6 0 ,f r z = 9 M , = 2 5 . 2M , z=25.5 Z = 1 . 1 6p , (Z)=0.247 D= 0.35,p(D)=0.245 U' -c a o L I E = z 'r5 10 15 Shelllength(mm) Fig. If . Size-frequencydistributions of G. palnleń; the white parts of bars representspecimenswithout scars and the gray pańs specimens with scars. Symbols: zl _ number of specimenswithout scans,n2 _ number of specimens with scars,Mt - median size of specimens without scars,Mz - median size of specimenswith scars,Z - statisticfor the Wilcoxon Median testwith normal approximationand continuity correction, p(Z) - significance of Z, D - Kolmogorov-Smirnov statistic, p(D) - significance of D. A. Locality One. B. Locality Two. cality) variation in frequency of attacked individuals among brachiopod patches. The apparentvariation among the three sampled patches is not statistically significant (Fig. 13). 516 FLESSA, Predatory scars: KOWALEWSKI, & MARCOT G = 4.08 P =0.130 d f= 2 n =325 c 8oo o IL 40 r Brachiopods withoutscars Brachiopods ffi with scars 0- Patch 1 Patch 3 Patch 2 Fig. 13. The variation in relative frequency of specimens with scars among three brachiopod patches sampledin November 1993in Locality One. The numbersabove eachbar representthe sample size of that bar. Symbols: G - log-likelihood ratio (G-statistic),p - significance of G, df - number of degreesof freedom,n - sample size. 154 G=29.8 P = 0.001 c o 172 180 G=2.9 P = 0.09 G = 32.3 P = 0.001 df=2 n=506 60 I o rL 40 r ffi lł::::łjił::::i::| lliiiiiiii$l 03.1993 11.1993 Brachiopods withoutscars Brachiopods with scars 02.1994 Fig. 14. The variation in relative frequencyof specimenswith scarsthroughtime (Patch 1, Locality One). The numbers above each bar representthe sample size of that bar. Symbols: G - log-likelihood ratio (G-statistic),p - significance of G, df - numberof degreesof freedom,n - sample size. 3. Variation in time. Patch 1 from Locality One was sampledthreetimes:in March 1993,in November 1993,and in February 1994.There is a significant variation in the frequencyof specimenswith scars across the seasons(Fig. 14). The frequencyof specimens with scars is substantially lower in the March 1993 sample than in the samples from the two subsequentseasons.There is no significant difference in the frequency of attacked specimensbetween November 1993 and February 1994 (for statisticaldetailsseeFig. 14). ACTA PALAEONTOLOGICA POLOMCA 42 (4) 5r7 Interpretation The origin of scars. - Despite severalweeks of observation,we have neverbeen able to directly observethe agentresponsiblefor scars,and thus,our interpretationof the origin of scars is somewhatspeculative.In addition,many abiotic and non-predatory biotic factorsexist that can causedamage,and consequently,repair scarsin shelly organisms.These include self-inflicted damage of burrowers and predators,abiotic damagedue to impactsof wave-bornestones,and humanactivity (for more details and referencessee Cadóe et aI. in press).Nevertheless,it seemsquite certainthat scars (1) arebiotic in origin; (2) record attemptsat predation;and (3) were madeby an epifaunal organismwith a scissors-typeweapon(e.g.,claws,beak). The small localized scars,thatcut acrossthe shell growthrings, clearly indicate an external agent of destruction.The evidence pointing to the biotic origin of scars includes the very limited size variation among the scars (Fig. a); their non-random distributionconcentratednearthe anteriorshell edge(Fig. 7); the fact thatit is possible to group scars into morphological types (Fig. 3; Table 2); and the presenceof complementary scars on opposite valves (Fig. 6). The non-randomdistribution of scars (Fig. 7), the overwhelming dominance of single scars (Table 2), and the correlation betweenshell size and scar size (in the case of u-shapedscars;Fig. 5) all suggestthe predatoryońgin of scars.The fact that scars concentratenear the anterior shell edge (Fig. 7) and, regardless of the scar type, open toward the anterior edge suggest predatoryattacksfrom the anterior side of the brachiopod.Lingulid brachiopodsare infaunal organismsthat live in vertical burrows and when active position themselves with their anterior-sideup and with their anteriorshell edge alignednearthe sedimentwater interface (e.9., E-ig 1982). Thus, the scars must have been produced by ar, epifaunal organism.The fact that many scars (again,regardlessof the morphological type of scar) consist of a pair of disruptions (Fig. 5) - that are of similar size and situatedon oppositevalves at a similar distancefrom the anteriorshell edge- suggest predatoryattackswith a scissors-typeweapon such as the claws of a crab or the beak of a bird. The identity of predator(s?). - The most likely epifaunal intertidal predators with a scissors-typeweaponinclude crabs and shorebirds(for review of shell-crushing predatorsseeVermelj 1987,1992).Both crabs and shorebirdsare commonin the study area. For several reasons, we believe that shorebirds are more likely predators.In particular,two speciesof sandpipersshould be considered:the willet, Catoptrophorus semipalmatus,and the long-billedcurlew Numeniusamericanus. Shorebirds, especially willets and long-billed curlews, are common in the study area(Wilbur 1987).They can, in fact,be extremelyabundantseasonally;coastalareas, from California to Peru are their wintering grounds (Johnsgard1981;Hayman et al. 1986;Wilbur t987; Richards 1988).Moreover,shorebirdstendto form denseaggregations when foraging (e.g.,Recher 1966), and thus, can account for the very high frequency of scars (Table 2). Finally, both long-billed curlews and willets are armed with long bills which makethemparticularlywell adaptedfor preying on lingulids. Bill length ranges from 113 to f19 mm in long-billed curlęws and from 50 to 67 mm in willets (Haymanet al. 1986).Becausewillets were observedpreyingonGlottidia and 518 Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT damagingthe anterior shell edge (Paine 1963) and because Glottidia has previously beenfound in the gut contentof willets (Paine 1963;Pereira1990),it seemsmore likely to us thatthe willet ratherthanthe long-billed curlew is responsiblefor the scars.There is, however,no direct emprical evidencewhich would allow us to decidethe predator's identity with certainty. For the same reason, crabs cannot be entirely excluded as possible predators.In contrast,shell-crushingfish such as rays - althoughpresentin the area,as indicatedby frequentray pits - should be excluded as possible predators. It seemsunlikely thattheir toothedjaws would generatealocalized andcomplementary pair of scars with regular outlines,even if we assumethatthey are able to capturefully infaunal organismssuch as Glottidia. Tlvo important caveats. - TWo concerns need to be stressedbefore proceeding with the interpretationof our data.First, as stressedabove,we are uncertainwhether the scars were all createdby one predatory species.Thus, the presenceof the three morphological types of scars may either suggestthat thereis more than one predator, or thatthereis a single predatorwhich producesmore thanone type of scar.[n thelatter case, the variation may be attributableto behavioral variation in predatoryattacksor in the response of the prey (see below). The data do not provide an unequivocal solution. The statistical similarities among the different scar types (i.e., similar size, distributionaroundthe anterioredge,similar dorso-ventraldistribution),may indicate that scars were made by one predator,but may also indic atea similar behavior (and weapon size) of two or more predators.Similarly, the anterior-posteriordifferencesin distribution of scar types (Fig. 9), can be used to argueeitherfor the presenceof two differentpredatorsthatpreyed on brachiopodsat differenttimes, or changesin predatory behavior with prey size. Second,repair scars record unsuccessfulpredationevents,and thus, are inherently difficult to interpret(see Schoener 1979;Schindel et al. 1982;Vermeij 1983;Walker & Voight 1994;CadÓeet al. in press).Most importantly'they cannotbe usedto estimate predationintensity:a prey population with f07o of repair scars may in fact be preyed upon at much higher ratesby an efficient predatoror at much lower ratesby a clumsy predator.In fact, some predatorsare known to repeatedlyattackunsuitableprey (e.g., Vermeij l98f), and thus, it is feasible that a'prey' with frequentrepair scars is never subjectedto predation.Also, if a predatoris (atleastoccasionally)successful,therepair scarsrepresentonly a subsampleof all attacks.Unless the unsuccessfuland successful affacks are the same in their ecological and behavioral aspects(e.g.,prey size, site of attack),a quantitativeanalyses of repair scars may provide misleading insights into predation.We will assumein the subsequentinterpretationthatthe repair scarsprovide representativesample for all attacks,but some alternativeinterpretationswill also be noted. Behavior of the predator. - If all, or mostof thescars,weremadeby one species of predator (e.g.,the willet), the variation in scar morphology reflects the variable foraging behavior of thatpredator.Stenzel et ąI, (1916),for example,observedwillets to display as much as five foraging behaviorswhen searchingfor prey: peck, multiple peck, probe, multiple probe, and theft. Changes in searching method may introduce variation in the strengthof the attack and the angle at which an attack is attempted. This, in turn, may affectthe morphology of a scar producedin an unsuccessfulattack. ACTA PALAEONTOLOGICA POLONICA 4f (4) 519 Alternatively, variation in the scar morphology may be a function of the prey escape response.G. palmeri is capableof rapid withdrawal into the deeperparts of its burrow with a surprisingstrength(personalobservations).According to our field observations (see also Kowalewski & Demko 1996), the G. palmeri burrows can easily exceed 50 cm. Thus, the depthof burrows exceedsnotably the length of the crab's claws and eventhelengthofthebillsof bothwillets(upto7 cm;afterHaymanetal.1986)and curlews(upto 22cm; afterHaymanetaL t986).It seemslikely thatboththecapturing methodof the predatoras well as the escaperesponseof G. palmeri is likely to change with brachiopod size. Indeed,the differencesin the anterior-posteriordistribution of different scar types (Fig. 10) suggestthat the variation in scar morphology may be relatedto brachiopod size. It is also possible that variation in scar morphology reflects variation in the crystallographyand mineralogyof the lingulid shell.The orientationof apatitecrystals, the orientationof organicmatrix, and proportionof organicto non-organicphasestend to vary strongly across the shell. In Lingula, for example, the length of the c-axis in apattte,the degreeof orientationof crystals, and proportion of apatiterelative to the organic matter all increase toward the shell center (Iijima et al. 1988; Iijima & Moriwaki 1990).Finally, as stressedearlier,variation in scar morphology may simply reflect the fact that thereis more than one speciesof predatorsthat attemptto prey on lingulids. Site-selectivedurophagouspredationcan be evaluatedby assessingrandomnessin the spatial distribution of predatorytraces on a shell. This line of evidence has been repeatedlyused for predatorydrillholes, both Recent and fossil (e.9.,Reyment 1971; Negus 1975;Kowalewski 1990;Anderson 1992).In case of our data,however,the non-randomdistributionof scars (Fig. 7) most likely reflects the fact thatthe direction of attackis strongly constrainedspatially: a shorebird(or crab) that attemptsto pull a brachiopodout of its burrow is most likely to seize the anteriorshell edge.In addition, the dorso-ventral distribution of scars (Fig. 6) does not suggest a valve-selective predation,and the distributionof scarsalong the anteriorshell edge(Fig. 7) also shows a lack of any site-selectivetendencies.Note, thatthe lack of site-selectivityis consistent with behavior of willets, which frequently prey upon infaunal organisms by randomly probing burrows or by detectingprey movementundęr water (e.g.,Stenzel et aI.1976). The correlationbetweenprey size and scar size (Fig. 5) may be used as an argument for size-selective predation.Note that although the correlation was found only for u-shapedscars,this most likely reflects thatfact that other scar types were all madein large specimens (Fig. 10); i.e., the independentvariable So varies so little that any potentialcorrelationcannotbe detected.It is, however,debatablewhetherthe scar size is well correlated with the predator size, and we have no rigorous data on the size-variationin shorebirdandcrab populationsin the area.A seeminglymore convincing argumentfor size-selectivity is provided by the strong correlation betweenprey size and the frequencyof attacks@ig. 9). Alternative explanationsexist here,however (e.g., Vermeij & Dudley 1982). First, larger/olderindividuals have potentially had more chance to encountera predatorthan the smallerĄounger ones. Second, a larger individual may be more likely to survive the attack than a smaller one becausethe damagedone by the predatoris smaller relative to the brachiopod size and, possibly, 520 Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT Ś20 g (U o a b15 o c o f Sro tL Distancefromanteriorshelledge(mm) Fig. 15. The anterior-posteńordistributionof scarson the brachiopodshell. Data the sameas in Fig. 9, but presented separately for each of the three sampling seasons (rhombs - March 1993, black circles Novembęr L993, x_ February 1994)' becausethe larger brachiopodsmay be able to withdraw their shell into their burrows with more strength. Seasonality of predation. - The most interesting and least ambiguous line of evidenceregardingpredatorbehavior is provided by the anterior-posteriordistribution of scars (Fig. 9). The significantly multimodal distribution suggestssubstantialvariation in predatoryattacksthroughtime.We believe thatthe modesreflect seasonal,late falVwinter predationattempts. The youngestmode is locatedat theanterioredge(Fig. 9). The distancedata,plotted separatelyfor each of the three sampling seasons(Fig. 15), indicate thatthis mode is presentboth in the November 1993 as well as the February 1994 samples.All scarsin the November 1993 anteriormode must have been made,thęrefore,in late Fall 1993, a shorttime before the collection of the samples.The scarsin the anteriormode of the February 1994 sample, may have also been made in the late Fall 1993 (G. palmeri ceases or slows its growth during the winter months; Batten & Kowalewski 1995; Anand et al. submitted),or during the 199311994Winter. The second anteriormode, both in the November and February samples,is located 3 mm from the anteriorshell edge.The distancebetweenthe modes coffespondsvery well to the annual growth of the G. palmeri populationof 2.4 mm (Table2). Thus, the secondmode colrespondsto ACTA PALAEONTOLOGICA POLONICA 42 (4) 52r the late Fall 1992 and/orWinter 1993.This is confirmed by the March 1993 sample which containsa significant mode at the anterioredge.When the March 1993 sample is corrected for growth, the mode coincides with the second anterior mode in the November 1993 and February 1994 samples(Fig. 15). Unfortunately,we do not have data on the brachiopodpopulationsprior to March 1993, and thus, we do not know how much the brachiopod populations grew in previous seasons.However, the growth ring analysis suggeststhat the two posterior modes coincide with seasonalgrowth rings (Batten& Kowalewski 1995;Anand et aI. submitted).Also, in all extantlingulids, the rate of growth slows down with increasing size/age(seeChuang 1961;Paine L963:Worcester1969;Kenchington& Hammond 1978),and consequently,the annual growth incrementsdecreasetoward the anterior shelledge.Thus, theincreasęin the distancebetweęnthemodesaway from the anterior shell edge (Fig. 9) strongly suggests that the two posterior modes also represent seasonal,falVwinter predation.The thfudmode, most likely, representsthe late Fall 1991 and/orWinter 1992 and the fourth mode the late Fall 1990 and/orWinter 1991. The seasonalpatternof predationrecordedin the anterior-posteriordistributionof scarsis consistentwith the hypothesisthatthe wintering shorebirdsare responsiblefor scars.Willets and curlews aremigratorybirds thatwinter on theoceaniccoastsof North and CentralAmerica (Johnsgard1981;Hyman et ąI.1986;Richards 1988).The coasts of Baja California and California are their major wintering grounds (Johnsgard1981; Haymanet aI. 1986;Wilbur 1987;Richards 1988).Those seasonalpopulationscan be extremely abundant and often become the dominant predator in the intertidal communities (Wilbur 1987).Moreover, migratory shorebirdssuch as willets are known to occasionallyremainin their winteringgroundsfor the entireyear (Haymenet al. 1986), which would accountfor thepresenceof somescarsin-betweenthe modes(Figs 9, 15). Impact on Glottidia populations. - Scars in live-collected specimens(or repair scars in fossil specimens) representunsuccessful predation attempts,and thus, as pointedout above,the frequencyof specimenswith scarsdoesnot necessarilycorrelate with predationintensity.Nevertheless,it is worth noting that the frequency of specimens with scars is high: comparableto the frequenciesobservedin modern mollusks (e.9.,Vermeij et aI. 1981)and higher than those observedin articulatebrachiopods (e.g.,Thayer& Allmon 1991).The high frequencyof brachiopodswith scarsmay mean thatshorebirds(or crabs)are very unsuccessfulpredatorsof lingulids and eithercannot learn from, or can afford, their frequentfailures. This 'clumsy-but-stubborn-predator modef is, however,inconsistentwith gut contentstudies (Paine 1963;Pereira 1990), that show that shorebtrdsare successful predatorsof lingulids. Thus, the high frequency of brachiopods with scars indicates, we think, a high intensity of predation (unless birds are successfulpredatorsand scars record an unsuccessfulpredationby crabs). The high predation intensity is corroboratedby the fact that specimenswith multĘle scarsare not frequentwhich suggests,in turn,a high rateof successfulattacks. Note also,thateven if all predationeventswere unsuccessful,the wound causedby the attackis likely to affectthe brachiopod'schancesof survival: unhealedscars are often found several mm away from the anterior shell margin suggestingthat brachiopods requiremonthsor even yearsto fully repair injuries causedby predators(alternatively, theseunhealedscarsmay have been fresh scarsmade away from the anteriormargin). 52f Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT At least four explanationscan be offeredfor the fact that specimenswith scars are significantly more frequent in Locality One than in Locality Two. First, the older populationsfrom Locality One (at least 3-4 years old; see Kowalewski 1996a;Anand et al. submitted)have had more opportunityto encountera predatorthan the younger populationsfrom Locality Two (1-2 yearsold). Thus, even if therewere no differences in frequency of attacks between the two localities, populations from Locality One would be expectedto include a higher proportionof specimenswith scars.Second,it is . possible that predatorsare more successfulwhen preying on smaller brachiopods. Third, when hunting predatorsmay select for larger preys (but see above). Finally, some subtle microhabitat differences betweenthe two localities - in particular, the substantiallyfiner granulometryof the intertidalsedimentin Locality TWo (seeKowalewski I996a)- may influence theintensityand effectivenessof foragingby predator's (especially shorebirds,see Quammen 1982). The increasein thefrequencyof specimenswith scarsthroughtime,betweenMarch 1993 and November 1993,most likely reflects the cumulative increasein specimens attacked by predators.In addition, the variation in predation intensity among the subsequentwinters and the increasedrate of failed attackswith increasedage of the brachiopod may also have contributedto the observedpattern.The available data are insufficient to evaluatethe relative importanceof those factors.The lack of variation in frequencyof specimenswith scarsamongthe threepatchesthatrangein microhabitat from the uppermostinteńidal to the lower middle intertidal (Kowalewski 1996a), suggeststhatpredatorsprey equally intensely in the upper and middle intertidal. Implications Biological implications. - Despite the many ambiguities that hamper the interpretationof repair sca.rs,we believe that our study indicates the existence of strong seasonalinteractionsbetweenshorebirds(and/orcrabs?)and inarticulatebrachiopods. Moreover, given the very high populationdensitiesof G. palmeri in the area (Kowalewski 1996a),not only may the shorebirds(and/orcrabs?)be an importantpredator of the brachiopod,but the brachiopodmay be an importantpart of the predatorsdiet, especially during the winter months. The predationon Recent articulatebrachiopodsis in generalmuch less intensethat thaton mollusks (e.g.,Thayer& Allmon 1991;Thayer 1985;Jameset al. 1992).This relatively lower predation intensity has been attributedto poor palatability and low energeticvalue of the articulatebrachiopods(Thayer 1985;Baliński 1993).This study suggests that in contrast to articulate brachiopods, lingulids are not repellent to predators.Indeed,a simple field experimentsuggeststhatthey may be a very palatable invertebrateprey: we fed live-collected specimens of G. palmeri to seagulls and observedthe sameindividual seagullhappily returningfor more. Our study is consistęnt with gut contentdata suggestingthatmany groupsof predatorseatlingulids (Paine 1963;Cooper 1973;Pereira I99O;Mason & Clugston 1993;Emig in press;Campbell & Campbell manuscript).Lingulids are also eatenby humans(e.9.,Stimpson 1860; Yatsu I90f; Emig in press),and in some areasthey form their'...favorite article of food...'(Stimpson1860:p. aafl. ACTA PALAEONTOLOGICA POLONICA 4f G\ 5f3 The data presentedhere suggestthat further biological research on brachiopodshorebird/crabinteractionsin the Colorado Delta may bring forth importantcontributions towardbetterunderstandingof the intertidalecosystemsof the innermostGulf of California. This may also prove importantfor understandingthe marine ecology and conservationbiology of nearshoremarineecosystemsin generalbecauselingulids can be very abundantin intertidal habitats (Emig 1983; Kenchington & Hammon 1978; Savazzi 1991;Kowalewski 1996a). Finally, this study shows thatrepair scarsmay offer insights into the seasonalityof predation,and thus, into the ecology of migratory animals and their impact on their transientecosystems. Paleontological implications. - Repair scars in lingulid shells may be preserved in the fossil record. This study shows that predators (most likely shorebirds) are capable of scarring the shells of a large proportion of the intertidal populations of G. palmeri. Moreover, repair scarsin Glottidia arealso known from at least two other localities:(1) the intertidalflats of the Gulf of Nicoya, Costa Rica (specimensof G. ąudebąrticollectedand providedto us by J.A. Vargas1996),and(2) theFlorida coast of the Gulf of Texas,USA (Paine 1963).Clearly, predatoryrepair scars are common in intertidalpopulationsof lingulids. Unquestionablelingulids (family Lingulidae) are known since the Late Devonian (Williams 1977) whereas sandpipers(order Chadriifonnes, family Scolopacidae)a monophyletic (Jehl 1968),exclusively predatoryfamily, which includes willets and long-billed curlews - are known from the fossil record since the Late Cretaceous (Brodkorb1963,I967).ThegenusNumeniusappearsin thefossil recordby theMiddle Miocene and thę genus Tringa (a close relative of Catoptrophorus)by the oligocene (Brodkorb 1967). Clearly, predatory shorebirds and lingulid brachiopods have coexisted in intertidal ecosystems since at least the middle Tertiary, but may have co-existedas early as the Late Cretaceous(molluscivorousbirds are known from the fossil record since at least the Late Eocene; Cracraft L973; Vermeij 19'77).Ttre shell-crushingability of modern predatory arthropods(e.g, stomatopods,spiny lobsters,crabs)may have evolvedin theLate Mesozoic or Paleogene(seeVermeij 19'77, 1987). Thus durophagousarthropods and lingulid brachiopods have co-existed in benthic ecosystemssince at least the early Tertiary. To our knowledge,however,repairScarshave neverbęenreportedin fossillingulids. This may be partly due to the fact that lingulids have very low fossilization potential (Worcester1969; Emig 1990; Kowalewski 1996a).Indeed,post-Jurassic lingulidshavevery poor fossil record(Kowalewski& Flessa 1996),andthus,arerarely preservedwell enough,or in a sufficient number,to allow for the recognitionof repair Scars.Also, and perhapsmore likely, fossil lingulids may have beenrarely examinęd for repair scars by paleontologists.We hope that the criteria and quantitativedata offered here will stimulatefuture paleoecologicalresearchon lingulids and will lead to the identification of repair scars in fossil lingulids. If repair scars in brachiopodsare predominatelymade by shorebirds,then specimens with scars may offer a useful paleoenvironmentalindicator as such brachiopods must have lived in the intertidal zone. The confinment of scarred specimens to intertidalpopulationsindeedseemsto be the casefor extantGlottidia.In the courseof 524 Predatoryscars: KOWALEWSKI, FLESSA, & MARCOT a morphometricproject (Kowalewshi et aI. 1997),we obtained specimensfrom six localities. Specimensfrom threeintertidallocalities (Localities One andTwo from Baja California, and one locality from Costa Rica) bear repair scars, whereas those from three subtidallocalities (musuemcollections form the subtidalof southernCalifornia, North Carolina, and the Gulf of Mexico) lack scars.This suggeststhatrepair scarsthat might be found in Tertiary fossil hngulids could be used as an evidence that those brachiopods lived in the intertidal environment;especially if other lines of evidence exist to suggestthat shorebirds were responsible for the scars. It should be noted, however,that scars were found in subtidalpopulationsof Lingula (C.C. Emig written communication 199"1). Because scars in the brachiopod shell can record seasonalpredationby migratory birds, the identificationof fossil populationsof brachiopodswith frequentrepair scars may be particularly exciting. Such populations may help in identifying seasonal predationin ancientmigratory birds. Because post-Jurassiclingulids have had a very low fossilizationpotential (Kowalewski 1996a;Kowalewski & Flessa 1996),they are less prone to time-averagingthan mollusks (Kowalewski 1996b, 1997), and thus, Tertiary lingulid assemblagesmay offer temporalresolution sufficiently fine for the analysis of seasonalpredation. In summary,we hope that this paper will stimulate paleontological research on predatory traces on lingulids - in particular, their implications for ecological and co-evolutionaryinteractionsbetweenlingulids and their predators. Acknowledgments This study was supported by the NSF grant EAR-94|7054 to Karl Flessa. Michał Kowa]ewski gratefully acknowledges support of the Alexander von Humboldt Foundation during the final stages of this project and thanks Wolfgang Oschmann and Jimmy Nebelsick from Ttibingen Universitiit for their hospitaliĘ. We thank Diana Hallman and Julie Anand for help at various stages of this project, Christian Emig for many useful comments and valuable information, and Andrzej Baliński and Gerhard Cadóe for carefuland helpful reviews of the final manuscńpt. This is publication number 26 of C.E.A.M. (Centro de Estudios de Almejas Muertas). References Alexander,R.R.l9S6a.Frequencyofsublethalshell-breakageinarticulatebrachiopodassemblagesthrough geologic time. In: P.R. Racheboeuf& C.C. Emig (eds),Les BrachiopodesFossiles et Actuels. Biostratigraphiedu Paleozoique4, 159-167. Alexander, R.R. 1986b.Resistanceto andrepair of shell breakageinducedby durophagsin Late Ordovician brachiopods. - J ournal of P al eontology 60,273-f85 . Alexander, R.R. 1990.Mechanical strengthof shells of selectedextantarticulatebrachiopods:implications for Paleozoic morphologic trends.- Historical Biolo gy 3, 169-1 88. Alexander, R.R. 1992.Survival and repair of the naturaland surgical damagein the articulatebrachiopod Terebratulina retusa (Linnaeus).- H istoric al B ioIogy 6, 22I -23 L Allmon, w.D., Nieh, J.C., & Nońs, R.D. 1990. Drilling and peeling of turritelline gastropodssince the Late Cretaceous.- Palaeontology 33, 595-61 1. Anand,J., Flessa,K.W., & Kowalewski,M. (submitted). inthe shellof theRecent Seasonalgrowthbanding lingulid brachiopod Glottidia p almeri DalI. ACTA PALAEONTOLOGTCA POLOMCA 42 (4) 5f5 Anderson,L.C. 1992.Naticid gastropodpredationon corbulid bivalves: effect of physical factors,morphological features,and statisticalartifacts.- Palaios 7,602-6f0. Anderson,L.C.,Geary,D.H.,Nehm,R.H.,&Allmon,W.D.l99l.Acomparativestudyofnaticidgastropod predation on Varicorbula caloosa and Chione cancellata, Plio-Pleistocene of Flońda, U.s.A. P alaeogeography, P alaeoclimatology, P alaeoecology 85, 283-f90. Baliński, A. 1993.A recovery from sublethaldamageto the shell of a Devonian spiriferoid brachiopod.Acta PalaeontologicaPolonica 38, 111-118. Batten,J. & Kowalewski, M. 1995.Seasonalgrowth banding and predationscarsin the shells of a Recent lingulide brachiopod.- Geological Society of America Abstracts with Prograrns 27 (6),A445. Batten,J., Chesley, K.B., Graybill, J.K., Marcot, J.D., Ramsey,M., Riley, B.C.D., Shinker,J.J., Smith, O.A., & Speer, J.H. 1994. Geomorphology, sedimentarystructures,and biota of the Lower Colorado delta, Baja California, Mexico. - University of Arizona Gesocience Symposium, Program and Abstracts1994,6. Bengtson, S. & Zhao, Y. 199f. Predatorial borings in Late Precambrian mineralized exoskeletons.Science257.367-369. Berg, J.C. 1976.Ontogenyof predatorybehavior in snails (Prosobranchia:Naticidae).- Nautilus 90, 1-4. Berg, J.C. & Nishenko, S. 1975.Stereotypyof predatoryboring behavior of Pleistocenenaticid gastropods. - Paleobiolo gy L, f58-260. Biernat, G. & Emig, C.C. 1993. Anatomical distinction of the Mesozoic lingulide brachiopods.- Acta P alaeontologic a P olonica 38, t-20. Bitner, M.A. 1996. Brachiopods from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula. In: A. Gaździckj (ed.), Palaeontological Results of the Polish Antarctic Expeditions. P alaeontologia P olonica 55, 65- 100. Bray, N.A. & Robles,J.M. 1991.Physicaloceanography of theGulf of California.łr: J.P.Dauphin& B'R.T. Simoneit (eds), The Gulf and Peninsular Provinces of the Californias. - American Association of P etroleumGeolo gistsBulletin 47, 5 11-553. Brodkorb,P.1963.BirdsfromtheUpperCretaceousofWyoming.-ProceedingsoftheXllllnteruational O rnithologic al C ongress 1,,55-70. Brodkorb, P.1967. Catalogue of fossil birds: Part 3 (Ralliformes, Ichthyornithiformes,Charadriiformes). - Bulletin of the Florida StateMuseum 11,,99-2f0. Bromley, R.G. 1981. Concepts in ichnotaxonomy illustrated by small round holes in shells. - Acta G eologic a Hisp anica 16, 55-64. Bromley, R.G. 1996. Trace Fossils: Biology and Taphonomy.Znded. 361 pp. Unwin Hyman, London. -Palaeontology 9,355-359. Brunton,H.1966.PredationandshelldamageinaViseanbrachiopodfauna. Brusca, R.C. 1980. CommonIntertidal Invertebratesof the GuIf of Califurnia.513 pp. University of Arizona, Tucson, USA. Cadóę, G.C. 1968. Molluscan biocoenosesand thanatocoenosesin the Ria de Arosa, Galicia' Spain. hologische VerhandelingenLeiden 95, I-LZI. . Cadóe, G.C. 1989. Size-selective transportof shells by birds and its palaeoecological implications. P al aeontology 32, 4f9 437 . Cadóe, G.C., Walker, S.E., & Flessa, K.W. (in press).Gastropod shell repair in the intertidal of Bahia la Choya. - P al aeogeog raphy,P al ąeoclimatology, P alaeoecology. Campbell, L.D. & Campbell, C.C. (manuscript).Distribution and paleoecology of Glottidia inexpectans Olsson (Brachiopoda:Lingulidae). Chatterton,B.D.E. & Whitehead,H.L. 1987.Predatoryborings in inarticulatebrachiopodArtiotretafrom the Silurian of oklahoma.- LethaiazU,67-ą4. Chuang, S.H. 1961. Growth of the postlarval shell in Lingula unguis (L.) (Brachiopoda).- Proceedings of the Zo ologic al Soc i ety of London 137, 299-3 lO. Cooper, G.A. 1973.Brachiopods (Recent).- Memoirs of the Hourglass Cruises 3, part 3, l-14. Marine ResearchLaboratory,Florida Departmentof Natural Resources. Cooper, G.A. 1988. Some Tertiary brachiopods of the East Coast of the United States.- Smithsonian C ontributionsto P aleobiology 64, I-54. Cracraft, J. 1973. Continental drift, palaeoclimatology,and the evolution and biogeographyof birds. Journal of Zoolo gy, London 169, 455-545. Dall, W.H. 1870.A revision of the Terebratulidaeand Lingulidae, with remarks and descriptionsof some recentforms' - American Journal of Conchology ó, 88-168. 5f6 Predatory scars: KOWALEWSKI, FLESSA, & MARCOT Dall, W.H. 1871. Supplement to the 'revison of the Terebratulidae', with additions, corrections and a revision of the Craniidae and Discinidae. - Ameńcan Journal of Conchology 7,39_79. Dall, W.H. 1920.Annotated list of the Recent brachiopodsin the collection of the United StatesNational Museum, with description of thirty-threenew forms. - Proceedings of the United StatesNational Museum57,f6I-377. Diaconis, P. & Efron, B. 1983. Computer-intensivemethodsin statistics.- ScientificAmerican 248, 116-130. Efron, B. 1979.Bootstrapmethods:anotherlook at thejackknife. - TheAnnals of Statistics7,I-26. Ekdale, A.A. 1985. Paleoecology of the marine endobenthos.- Palaeogeography,Palaeoclimatology, Palaeoecology 50,63-8 1. Emig, C.C' I98f. Terrier et position des Lingules (Brachiopodes,Inarticulós). - Bulletin de la Socićtć Zoologiquede France 107, 185-194. Emig, c.C. 1983. Taxonomie du genre Glottidia (Brachiopodes,Inarticulós).- Bulletin de Museum nationaled'Histoire naturalle,Paris 4 (5),sectionA(f),469489 Emig C.C. (in press).Ecology and biogeographyof the inarticulatedbrachiopods.In; R.L. Kaesler (ed.), Treatise on InvertebratePaleontology, Part H, Brachiopoda, 1. Geological Society of America and University of Kansas Press, Boulder Colorado, and Lawrence Kansas, USA. Emig, C.C. & Vargas,J.A. 1990.Glottidiaaudebarti(Broderip),(Brachiopoda,Lingulidae)from the Gulf of Nicoya, Costa Rica. - Revistade BiologiaTropical3S,25I-258. Emig, C.C., Gall, J.C.,Pajaud,D,, &Plaziat,I,C.1978'Róflexions critiquessur1'ócologieetlasystómatique des lingulesactuelleset fossiles.- Gćobios|t,573_609. Ezcurra, E. & Rodrigues, V. 1986.Rainfall patternsin the Grand Desierto, Sonora,Mexico. - Journal of Arid Environments10, 13-28. Fairweather,P.G. 1985. Differential predation on alternativepreys, and the survival of rocky intertidal organismsinNewSouthWales.-Journalof ExperimentalMarineBiologyandEcology 89,135-156. Flessa,K.w., Kowalewski,M., & Walker, s.E. 1992.Post-collectiontaphonomy:shęlldestructionandthe Chevrolet. - Palaios 7, 553-554. Ftirsich, F.T. & Jablonski, D. 1984. Late Triassic naticid drillholes: carnivorous gastropodsgain a major adaptationbut fail to radiate.- Science 224,78-80. Garrity, S.D. & Levings, S.C. 1981.A predator-preyinteractionbetweentwo physically and biologically constrained tropical rocky shore gastropods:direct, indirect and community effect. - Ecological Mono graphs 5I, f67 -f86. Geary,D.H., Allmon, W.D., & Reaka-Kudla,M.J. 1991.Stomatopodpredationon fossil gastropodsfrom the Plio-Pleistoceneof Florida.- Journal of Paleontology65,355-360. Hatai, K. 1938. on some Cenozoic Brachiopoda from the North American region. - Ameńcan Midland N aturali st L9, 7 06-7 2f . Hayman, P., Merchant, J., & Prater,T. 1986.Shorebirds:An IdentfficationGuide to Waders of the World. 4Lf pp. Crrom Helm, London. Hertlein, L.G. & Grant IV, U.S. 1944.The Cenozoic Brachiopoda of westernNorth America. - University of Califurnia Los Angeles Publications in Mathematical and Physical Sciences 3,I-f36. Hoffman, A., Pisera, A., & Ryszkiewicz, M. 1974. Predation by muricid and naticid gastropodson the Lower Tortonian mollusks from the Korytnica Clays. - Acta Geologica Polonica 24,f49-f60. Hoffman, A. & Martinell, J. 1984. Prey selection by naticid gastropods in the Pliocene of Emporda (NortheastSpain).- Neues Jahrbuchfiir Geologie und Paliiontologie, Monatshaft L984,393-399 . Iijima, M. & Moriwaki, Y. 1990. Orientation of apatite and organic matrix in Lingula unguis shell. Calcifted Tissue International47, f31-f4f . Iijima,M., Moriwaki, Y., Doi, Y., & Kuboki, Y. 1988.The orientationof apatitecrystalsinLingulaunguis shell. - JapaneseJournal of Oral Biology 30,f0-30. James,M.A., Ansell,A.D., Collins,M.J., Curry,G.B., Peck,L.S., & Rhodes,M.C.I99f . Biology of living brachiopods.- Advances in Marine Biology 28,175-387 . Jehl, J.R., Jr. 1968.Relationshipsin the Charadńi (Shorebirds):a taxonomic study basedon color patterns of the downy young.- San Diego SocieĘ of Natural History Memoir 3, I_54' Johnsgard,P.A. 1981.ThePlovers, Sandpipers,and Snipesof theWorld.49f pp.The University of Nebraska Press,Lincoln, Nebraska. Kabat, A.R. 1990. Predatory ecology of naticid gastropodswith a review of shell boring predation.Malac ologia 32, 155-193. ACTA PALAEONTOLOGICA POLONICA 4f G) 521 Kelley, P.H. 1989. Evolutionary trends within bivalve prey of ChesapeakeGroup naticid gastropods.Histońcal Biolo gy 2, 139_156' Kelley, P.H. 1991. The effects of predation intensity on rate of evolution of five Miocene bivalves. Historical Biology 5, 65-78. Kelley, P.H. & Hansen, T.A. 1996. Naticid gastropodprey selectivity through time and the hypothesisof escalation.- P alaios 11.540-556 Kenchington, R.A. & Hammond, L.S. 1978. Population structure,growth and distribution of Lingula anatina (Brachiopoda)in Queensland,Australia. - Journal of Zoology, London 184, 63-81. Kitchell, J.A. 1986.The evolution of predator-preybehavior:naticid gastropodsand their molluscanpreys. In: M.H. Nitecki & J.A. Kitchell (eds), Evolution of Animal Behavior: Paleontological and Field Approaches, 88-1 10. Oxford, New York. Kitchell, J.A., Boggs, C.H., Kitchell, J.F., & Rice, J.A. 1981. Prey selectionby naticid gastropods: experimentaltestsand application to the fossil record.- Paleobiology 7,533-552. Kowalewski, M. 1990.A hermeneuticanalysis of the shell-drilling gastropodpredationon mollusks in the Korytnica Clays (Middle Miocene; Holy Cross Mountains, Central Poland). - Acta Geologica Polonica 40. I83-fI3. Kowalewski, M. 1993.Morphometric analysis of predatorydrillholes. - Palaeogeography,Palaeoclimatolo gy,P alaeoecology L02, 69-88. Kowalewski, M. 1996a.Taphonomyof a living fossil: thelingulide brachiopodGlottidia palmeriDall from Baja California,Mexico. - Palaios 1I,f44-265. Kowalęwski, M. 1996b. Time-averaging, overcompleteness,and the geological record. - Journal of Geology 104,3I7-3f6. Kowalewski,M. 1997. The reciprocal taphonomicmodel. - Lethaia 30, 86-88. Kowalewski, M. & Demko, T.M. 1996.Trace-fossils and population paleoecology:comparativeanalysis of size-frequencydistributionsderivedfrom burrows.- Lethaia29,II3-124. Kowalewski, M. & Flessa, K.W. 1994. A predatory drillhole in Glottidia palmeri Dall (Brachiopoda; Lingulidae) fromRecent tidal flats of northeasternBajaCalifornia,Mexico. -Journal of Paleontology 86.1403-1405. Kowalewski, M. & Flessa, K.W. 1995. Comparative taphonomy and faunal composition of the shelly cheniersfrom the northeasternBaja California, Mexico' - Ciencias Marinas 21',ś5_177. Kowalewski, M. & Flessa, K.w. 1996.Improving with age:the fossilręcord of lingulide brachiopodsand the natureof the taphonomicmegabiases.- Geology24,977-980. Kowalewski,M., Flessa,K.W., & Aggen,J.A.1994. Taphofaciesanalysisof Recentshellycheniers(beach ridges),northeasternBaja California, Mexico. - Facies 3L,209-f4f . Kowalewski, M., Dyreson,E., Marcot, D., Vargas, J.A., Flessa, K.W., & Hallman, DP. 1997.Phenetic discriminationof biometric simpletons:paleobiologicalimplications of morphospeciesinthe lingulide brachiopod Glottidia. - P aleobiology 23, 444469. Kropp, R.K. 1992.Repaired shell damageamong soft-bottommollusks on the continentalshelf and upper slopenorthof Point Conception,California.-Veliger 35, 36-51. Lowe, H.N. 1933.At the head of the Gulf of California. - Nautilus 47, 4547. Mason, W.T., Jr. & Clugston, J.P. 1993. Food of the Gulf Sturegoenin'the SuwanneeRiver, Florida. Transactionsof theAmerican Fisheries SocieĘ 122,378_385. Miller, R.H. & Sundberg,F.A. 1984.Boring Late Cambrianorganisms.- Lethaia17,185-190. Neugus, M. 1975. An analysis of boreholes drilled by Natica catena (da Costa) in the valves of Donax vittatus(da Costa).- Proceedings of theMalacological Society of London 4L,353-356. -Science241', Norton,s.F. 1988.Roląofthegastropodshelloperculumininhibitingpredationbyfishes. 9f-94. Paine, R.T. 1963. Ecology of the brachiopod Glottidin pyramidata. - Ecological Monographs 33, r87-f13. Pereira,A.I. 1990.Ecologfa de la alimentación de Limnodromusgriseus, Catoptrophorussemipalmatusy Numeniusphaeopus(Aves, Scolopacidae)en Chomes,Costa Rica. M.Sc. Thesis,Universidad de Costa Rica. Quammen, M.L. 1982. Influence of subtle substratedifferences on feeding by shorebirds on intertidal mudflats.- Marine Biology 71,339-343. Recher, H.F. 1966. Some aspectsof the ecology of migrant shorebird.- Ecology 47,393407. Reyment,R.A. 1971.IntroductiontoQuantitativePaleoecology.ffT pp. Elsevier,Amsterdam. 528 Predatorv scars: KOWALEWSKI. FLESSA. & MARCOT Richards,A. 1988.BirdsoftheTideline:ShorebirdsoftheNorthernHemisphere.2f4pp.DragonsWorld, Surrey,England. Robba, E. & Ostinelli, F. 1975.Studi paleoecologici sul Pliocene Ligure. I. Testimoniaze dipredazione sui molluschi Pliocenici de Albenga. - Rivista Italiana di Paleontologia e StratigrafiaBL,309-372. Roden, G.I. 1964.Oceanographicaspectsof the Gulf of California . In: T .H. van Andel & G.G. Shor (eds), MarineGeologyof theGulf of California.-AmericanAssociationof PetroleumGeologistsMemoir 3,30-58. Rowell, A.J. 1965. Inarticulate.In: R.C. Moore (ed.), Treatise on InvertebratePaleontology, Part H, Brachiopoda 1,}l260-Hf96. Geological Society of America and University of Kansas Press,Boulder, Colorado and Lawrence, Kansas, USA. Ruggiero, E.T. 1991.A study of damageevidence in brachiopod shells. In: D.I. MacKinnon, D.E. Lee, & J.D. Campbell(eds),BrachiopodsThroughTirne,203-210.Balkęma,Rotterdam' SAS Institute.1989. SASISTAT User's Guide (version 6), 4th ed. 943 pp. (vol. 1), 846 pp. (vol. 2), SAS Institute,Cary, USA. SAS Institute.1990a. SAS Procedures Guide (version 6),3d ed. 705 pp. Sas Institute,Cary, USA. SAS Institute.1990b.SAS/IML.235 pp. Sas Institute,Cary, USA. SAS Institute1991. SASl-anguageGuide.755 pp. Sas Institute,Cary, USA. Savazzi,E,199L. Burrowing in the inarticulatebrachiopodLingulaanątina, - Palaeogeography,Palaeoclimatology,P alaeoecology 85, 10 1-106. Schindel, D.E., Vermeij, G.E., & Zipser, E. 198f. Frequencies of repaired shell fractures among the Pennsylvaniangastropodsof North-Central Texas. - Journal of Paleontology 56,729-:140. Schoener, T.W. 1979. Infening properties of predation and other injury-producing agents from injury frequencies. - Ecology 60, 1110-1 115. Sheehan,P.M. & Lesperance,P. 1978. Effects of predation on the population dynamics of a Devonian brachiopod. - Joumal of Paleontology 52,812-817. Smith, O.A., Hallman, D.P., & Batten, 1.1995. Comparative taphonomy of Recent lingulide brachiopod and bivalve shells:an experimentalstudy.- Geological Society of America Abstracts with Programs 27 (6),A-135. Stenzel, L.E., Huber, H.R., &Page, G.W. 1976. Feeding behavior and diet of the long-billed curlew and willet. - The Willson Bulletin 88, 3 15-332. Stimpson,W' 1860.A trĘ to Beaufort,N. Carolina. - American Journal of Science 29,2nd series,44f445 . Sykes, G.G. 1937.The Colorado Delta. - Carnegie InstitutionWashingtonPublication 460,1-193. Taylor, J.D., Morris, N.J., & Taylor, C.N. 1980. Food specialszationand the evolution of predatory prosobranchgastropods.- P al aeontology 23, 375 409 . Thayer, C.W. 1985.Brachiopods versusmussels:competition,predation,andpalatability. - Science228, r5f7-15f8. Thayer, C.W. & Allmon, R.A. 1991. Unpalatable thecideid brachiopods from Palau: Ecological and evolutionaryimplications.In:D.I.MacKinnon, D.E. Lee, &J.D. Campbell(eds\,BrachiopodsThrough Time, 26I-264. Balkema, Rotterdam. Thayer, C.W. & Steele-Petrovic,H.M. 1975.Burrowing of the lingulid brachiopod Glottidia pyramidata: its ecologicand paleoecologicsignificance.- Lethaia8,f09-221. Thomas, R.D.K. 1976.Gastropodpredationon sympatricNeogene speciesof Glycymeris (Bivalvia) from the easternUnited States.- Journal of P aleontology 50, 488499. Thompson, R.W. 1968. Tidal flat sedimentationon the Colorado River delta, nońhwestern Gulf of California. - Geological Society of America Memoir L07, 1-133. Thomson, D.A. (ed.) 1993. 1993 Tide calendar for the northern Gulf of Caltfurnia. [No page numbers]. Printing and Publishing Support Services, University of Arizona, Tucson, USA. Treuman,E.R. &Wong, T.M. 1987.Theroleofthecoelemasahydrostaticskeletoninlingulidbrachiopods. - Journal of Zoology, London 2L3, 22I-23f . Vale, F.K. & Rex, M.A. 1988.Repaired shell damagein deepseaprosobranchgastropodsfrom the western North Atlantic. - Malacologia 28, 65-79. Vale, F.K. & Rex, M.A. 1989. Repaired shell damagein a complex of ńssoid gastropodsfrom the upper continentalshelf southof New England. - Nautilus 103, 105-108. Vermeij, GJ.1977. The Mesozoic marine revolution: evidence from snails, predators and grazers. P aleobiology 3, f45258. Vermeij, G.J. 1982.Gastropodshell form, breakage,and repairin relationto predationby the crab Calappa. - Malacologia23,l-12. ACTA PALAEONTOLOGICA POLONICA 42 G\ 529 Vermeij, G.J. 1983. Traces and trends in predation, with special reference to bivalved animals. P alaeontology 26, 455465 . Vermeij, G.J. 1987.Evolution and Escalation.52T pp. Princeton University, Princeton. Vermeij, GJ. 1992.A Natural History of Shell.fOT pp. Princeton University, Princeton. Vermeij, G.J. & Dudley, E.C. 1982. Shell repair and drilling in some gastropodsfrom fupley Formation (UpperCretaceous)of the South-eastern U.S.A. - Q7ę76ęęgus Research3,397403, Vermeij, G.J., Zipser, E., & Dudley, E.C. 1980.Predationin time and space:peeling and drilling in terebrid gastropods.- P aleobiology 6, 352-364. Vermeij, G.J., Schindel, D.E., & Zipser, E. 1981. Predation through geological time: evidence from gastropodshell repair.- Science 214, I0f+-I026. Vermeij, G.J.,Zipser,E., &Zardini, R. 1982.Breakage-inducedshell repairin some gastropodsfrom the upperTriassic ofltaly. - Journal ofPaleontology 56,233-f35. Walker, S.E. & Yamada, S.B. 1993.Implicationsfor the gastropodfossil record of mistakencrab predation on emptymollusc shells.- Palaeontology36,735-74L. Walker,S.E. &Voigt,J.R. 1994.Paleoecologicandtaphonomicpotentialof deepseagastropods.-Palaios 9,49-59. Wiedman,L.A., Feldmann,R.L., Lee, D.E., & Zinsmeister,W.J. 1988.Brachiopodafrom the La Meseta Formation (Eocene),Seymourlsland,Antarctica.ln: R.M. Feldmann& M.O. Woodburn (eds),Geology and Paleontology of the Seymour Island, Antarctic Penninsula. - Geological Society of America Memoir 169,531-539. Wilbur, S.R. 1987.Birds of Baja Califurnia. 253 pp.University of California,Berkeley,USA. -Journal Wiltse,W.L l9S0.PredationbyjuvenilePolinicesduplicatus(Say)onGemmagemma(Totton). of ExperimentalMarine Biology and Ecology 42, t87-199. Worcester,W. 1969.On Lingula reevei.Unpublished Master Science Thesis. 49 pp.University of Hawaii, Hawaii. Yatsu, N. 1902.On the habitsof the JapaneseLingula. - AnnotationeszoologicaeJaponensis4,61-67 . Zar,J.H. L984.BiostatisticalAnalysis.718 pp. Prentice,Englwood Cliffs. Appendix 1 The Monte-Carlo model based on the Poisson distribution. The SAS program (for SAS release 6.11) that performs the procedure described here is available upon request from M. Kowalewski. The approach proposed here is based on the method described by Reyment (I91L) to analyze the spatial distribution of predatory marks. In contrast to the Reyment's approach, we employ here a non-parametric, computer-intensive technique that would not have been feasible 25 years ago, when the Reyment's approach was published. The test evaluates whether the spatial distribution of scars is different from random. In this approach, the scar-frequency distribution calculated for the acfual data was compared to the distńbution expected for random data predicted by the Poisson distribution with mean 1,. ?u= N/s where fu- poisson distribution mean; N- number of scars; and s - number of sectors. (1) A given scar-frequency distribution includes s observations where N equals: s l,r=Dt (f) i=I where y is a number of scars in an i-th sector.Consider a3x3 grid of 9 sectorsthat contains 7 scars. Suppose, for example, that there is 1 sector with 3 scars, 4 sectors with 1 scar, and 4 sectors with 0 scars. The scar-frequencydistribution is thus based on 9 observations(3,1,1,1,1,0,0,0,0) that sum up to 7. The null hypothesis that the data have a random spatial distribution can be evaluated by comparing the sector-frequency distribution to the theoretical distribution predicted by Poisson 530 Predntory scars: KOWALEWSKI, FLESSA, & MARCOT function with l" = N/s. In the above example of 9 sectors and 7 scars, the expected distribution should be calculated for ?u= 0.7778. The significant difference between the actual distribution and the expected distribution Ęects the null hypothesis that data came from the population with a random spatial distibution. In Reyment's approach the two disfributions are compared directly using the X2 statistic. However, such an approach requires an arbitrary a priori lumping of the categories that contain small percentage of observations (Reyment I97I) and also requires assumptions of )P test which can be avoided when using a computer-intensivemethod (e.g.,Diaconis & Efron 1983). Our approach consists of the following steps: Step 1. 10 000 random datasetswith sample size s, are drawn from the Poisson distribution with mean 1,,where fu is calculated from the actual data. In the simulation, we used the Poisson function provided by SAS (see SAS 1991). Step 2. Each of the random datasetsis compared to the expected Poisson disfribution with mean 1,. The difference between the two distribulions is estimated by G (a log likelihood ratio), the parameter which is often considered superior to the -X2statisticr). G=2ź,,,,'E&) (3) where G - likelihood ratio, f(i)o -nvntber of observation in category i, f(i)" - number of expected observation in category i as expected from Poisson distribution. Note, that 10 000 G-values deńved in the simulation provide an estimate of the probability distribution for random datasets with sample size s drawn from Poisson function with a mean 1". Step 3. A single G-value for the actual data is calculated using the sź}meexpected Poisson distribution as used in Step f. The probability associated with the obtained G-value (p) is then estimated using empirical dishibution of G-values obtained in Step 2. We used the percentile method (also called nave bootstrap approach, see Efron 1979): (4) P=x/i where p - is probability that data came from a Poisson-distributed population, x - z number of randomly derived G-values greater than or equal to the G-value calculated for the actual data, and i - number of iterations (10 000 in our case). Note that i defines the number of decimal places that can be reportedforp; when p = 0, thenp <Ili (i.e.,0.0001in our case). 1) Note, thatthe choice of the goodness-of-fitstatisticis not cńtical in our app1oachbecausethe probability function is built empirically through a Monte-Carlo simulation.Thus, X, or Kolmogorov-Smirnov D could be used equally successfullyin our approach. Appendix 2 Bootstrap procedure for local significance of modęs (employed here to analyze data presented on Fig. 10). The program written in SAS/IMLis available upon request from M. Kowalewski. In order to assessthe statistical significance of multiple modes in a single distńbution, we propose here a simple bootstrap procedure. The procedure estimates the probabiliĘ of whether a given mode is locally significant - i.e., significant in respect to the directly adjacent bins (frequency classes) or locally insignificant (i.e., could be produced by sampling of a population which lacks that mode). The procedure is based on the resamptng of the actual data according to the following protocol. Step 1. The modes to be evaluated are identifiedt in the original data (in ow case, 4 modes indicated on Fig. 10). Step 2. A sample (in our case 203 distance measurements presented on Fig. 10) is resampled with replacement. The resulting bootstrap sample is used to calculate a new frequency distribution. ACTA PALAEONTOLOGICA POLOMC A 4f (4) 531 Each mode is then evaluated according to the simple cńterion. If the number of observation in the mode is greater than in any of the two adjacent frequency-classes, thę bootstrap sample is assigned '1'. ff any of the two adjacent classes has equal or greater number of observation than the value of '0'. mode, the sample is assigned value of Step 3. Step 2 is repeated n number of times. In our analysis łz= 10,000. The null hypothesis for a given mode is rejected2)if p < 0.05. Wherep (probabilĘ that sample came from a population 'mode' has fewer or equal number of observations than at least one of the two directly where the adjacent bins) is given by the following formula: p = 1 .- L where x - number of bootstrap samples ,l*.n n - number of iterations. (1) were assigned 'f in the procedural Step 2, and 1) Note that position and height of modes dependon how we define the bins. In case of our data,bins are 1-mmintervals(Fig. 10). 2) Although the analysis evaluates four hypothesis, the tests are dependent(i.e., based on the same bootstrapsamples)and Bonferroni correctionshould not be applied. współczesnego w muszlach Blizny drapieżnicze ram ie nio no ga lin gulidowe go Glo ttidia p almeri giczne i ekolo giczne paleontolo i ich znaczenie MICHAŁ KowALEwsKI. KARL w. FLEssA i JoNATHAN D. MARCoT Streszczelnie Szczegótowa ana|izailościowabLtzndrapiezniczych w muszli ramienionogabezza. wiasowego Z grupy lingulidów opartajest na 8f0 okazach Glottidia palmeri Dall, 1870. Okazy Zebrano z dwóch stanowisk z równi międzypływowych pótnocnowschodniĄ Zatokl Kalifornijskiej w Meksyku. Blizny drapieznicze występują w kiesze23.4%o osobników.Mozna je podzieLtćnaczterykategorie:blizny u-kształtne, Niezaleznieod ich morfologii,blizny koncentĄą niowe, spękaniowęorazpozostałe. jest rozwartąStroną się przy przedniejkrawędzimuszli. Większośćb|iznzorientowana w kierunku przedniej krawędzi muszli i wiele z nich składa się z dwóch b|izn zlokalizowanych naprzeciwlegle nabr^Bznej i grzbietowejskorupceramienionoga. (1) blizny wahająsię w wielkościod 1,5 do 24 mmf Analizailościowawskazuje,źLe _f,5 mmz;iwszystkiecztery kategorieblizn*ająpodobnerozkładywielko(średnia ści;(f) rozI7l7eszczeniebliznna powierzchni muszli nie jest losowe, podczasgdy ich rozkład grzbieto-brzaszny wydaje się być losowy; (3) proporcja zagojonych b|izn wzrastaw kierunku tylnej częścimuszli; (4) rozkładblizn jest udetza1ącomultimodalny i sugerujesezonalnedrapieznictwoskoncenffowanepóźnąjesieniąizimą; (5) częokazów zbliznamt stośćbltznwzrasta wraz z wielkościąramienionoga;i (6) częstość waha się znaczącopomiędzy dwoma badanymi stanowiskami,jak również'w obrębie stanowiska 1 w czasie, ale nie waha się znacz4co pomiędzy różnymi miejscami opróbowania w obrębiestanowiska1. 53f Predatory scars: KOWALEWSKI. FLESSA. & MARCOT Blizny repręZentująnieudane ataki jakiegośepifaunalnego drapieznika, wypoSazonegow nozycowy narząd chwytny (np. szczypce kraba, dzi6b ptaka). Wysoka częstość ataków, ich sezonalność i poprzedniebadaniaekologiczne zgodnie sugeruj4, żeb|iznys4 wynikiem ataków drapieznychptaków (Catoptrophorussemipalmatus|ub Numeniusamericanrzs). WybrzeiaPó|wyspu Kalifornijskiegosąmiejscemzimowania drapieznych ptaków i goszczą ich liczne populacje. Nie moinajednak całkowicie wykluczy ć,że drapieznikamibyłykraby.Poniew aŻbltznyreprezentuj4 nieudaneataki, ilościowe ana|izy dotycząceselektywnościmiejsca ataku, selektywnościwielkości ofiary i wpływu drapieznictwa na dynamikę populacji ramienionoga są trudne do j ednoznacZnego zinterptetowania.Niemniej j ednak, wyniki sugerują istnienie silnej sezonalnej za|eźzności ekologicznej pomiędzy ptakami (krabami?) i ramienionogami. Ana|tzailustruje metodyilościoweuiyteczne w badanichwspółczesnychi kopalnych bltzn drapieźLniczych i ma istotneimplikacje paleontologiczne.Drapiezneptaki, k.aby i ramienionogi mogły współzamieszkiwać strefy mtędzypływowepocząwszy od późnegomezozoiku. Tak więc, blizny drapiezniczew muszlachramienionogów mogą mieć długizapis kopalny, interesuj4cydla paleontologii, szczególnie z punktu widzenia paleoekologii ewolucyjnej.PoniewaŻblizny w muszlach linguIidów pozwilujq rozpoznać sezonalne drapieznictwo, kopalne blizny mogą potencjalnie dostarczyć danych ekologicznych i etologicznych,które sąZazwycza1rzadkodostępnew paleontologii.
© Copyright 2024