Scorpion taphonomy: criteria for distinguishing fossil scorpion molts and carcasses.
The ability to distinguish fossil arthropod carcasses from their
molts is necessary for a more complete understanding of the arthropod
fossil record and for more accurately assessing the role of fossil
arthropods in paleoecosystems. Taphonomic characteristics, e.g.,
recurrent patterns of disarticulation of exoskeletal elements, are the
primary data that have been used to differentiate fossil exuvia and
fossil carcasses among arthropods. This study documents recurrent
taphonomic patterns in modern scorpion carcasses and molts and extends
these patterns to the fossil record to define criteria by which fossil
scorpion molts might be distinguished from fossil scorpion carcasses.
The three most useful and statistically significant characters in making
the scorpion carcass/molt distinction are: position of the chelicerae
(drawn in or extended); position of walking legs (folded or splayed);
and body line (straight or curved). Two other characteristics, the
position of pedipalps and presence or absence of telescoped segments,
approach statistical significance and are also potentially useful.
Disarticulation data are not as useful for distinguishing fossil
scorpion molts and carcasses, because there are no statistically
significant differences in length of time to total disarticulation or in
the sequence of disarticulation between scorpion molts and carcasses.
Among extant arthropods, scorpions possess the body plan most similar to
that of the extinct eurypterids. Therefore, the taphonomic criteria
developed for distinguishing fossil scorpion molts and carcasses may
have implications for understanding molting among eurypterids.
Keywords: Arthropod, ecdysis, eurypterid
Animals, Fossil (Identification and classification)
Scorpions (Physiological aspects)
McCoy, Victoria E.
Brandt, Danita S.
|Publication:||Name: The Journal of Arachnology Publisher: The American Arachnological Society Audience: Academic Format: Magazine/Journal Subject: Biological sciences; Zoology and wildlife conservation Copyright: COPYRIGHT 2009 The American Arachnological Society ISSN: 0161-8202|
|Issue:||Date: Sept, 2009 Source Volume: 37 Source Issue: 3|
|Topic:||Event Code: 310 Science & research|
|Geographic:||Geographic Scope: United States Geographic Code: 1USA United States|
Scorpions are terrestrial chelicerates that have a fossil record
extending back more than 400 million years to the Silurian Period.
Fossil scorpions, although relatively rare, can be well preserved (Menon
2006). However, the relative importance of fossil scorpions in ancient
ecosystems is difficult to assess because of the arthropod trait of
growth through ecdysis. An individual scorpion may accumulate a number
of molts over its lifetime; these molts may not be distinguished easily
from carcasses, especially after becoming fossils, thereby complicating
interpretation of the scorpion fossil record. This is also the case with
fossil horseshoe crabs (Chelicerata: Xiphosura), whose fossil carcasses
and molts are often indistinguishable (Babcock et al. 2000). Therefore,
for many fossil arthropod taxa, simple or apparent abundance may not be
a reliable reflection of actual abundance. Without accurate abundance
estimates, it is difficult to determine the importance of these
arthropods in paleoecosystems.
There are a number of differences between modern scorpion molts and carcasses, such as the presence of internal organs in carcasses and the lack of most of these structures in exuvia, but differences based on internal anatomy are not readily apparent in fossils; indeed, internal structures usually cannot be discerned in fossil scorpions (but see: Wills 1925, 1946, 1960; Kjellesvig-Waering 1986). External features of the exoskeleton, such as the presence or absence of appendages, opened sutures, and dislocations (separations) between segments, are more readily accessible characters for making the potential distinction between carcasses and exuvia among fossil arthropods. These kinds of taphonomic observations of the scorpion exoskeleton are the focus of this investigation. The purpose of this paper is twofold: 1) to document whether different taphonomic patterns exist between modern scorpion carcasses and molts; and 2) to use these patterns, if present, to develop criteria for distinguishing fossil scorpion molts from carcasses.
PREVIOUS WORK ON SCORPION MOLTING AND TAPHONOMY
Scorpion molting is well understood (Polis 1990; Brownell & Polis 2001; Gaban & Farley 2002). The steps scorpions follow during molting do not appear to vary significantly among taxa (Rosin & Shulov 1962; De Armas 1986): the anterior suture opens and the animal moves forward to exit the old exoskeleton, in a manner similar to that of a horseshoe crab (Shuster 1982). A scorpion exuvium may include the booklung lamellae, preoral tube, and other internal features and there may be little distortion of delicate hairs, bristles, and setae (Gaban & Farley 2002). The exuvium is commonly intact except for a wedge-shaped gap beneath the carapace (Gaban & Farley 2002). These observations on modern scorpion exuvia suggest that, as in the case of horseshoe crabs, a well-preserved fossil scorpion exuvium may be difficult to distinguish from a well-preserved fossil scorpion carcass. In this study, we identify more readily observed external features of the scorpion exoskeleton as the basis for distinguishing scorpion molts and carcasses.
Six species of living scorpions belonging to six genera were used in the taphonomy experiments (Table 1). These taxa were chosen because they were available in sufficient quantity for replicate experiments. The scorpion molts used in this study were donated by arachnid hobbyists; live scorpions were purchased through a commercial supplier (www.swiftinverts. com) or were donated by arachnid hobbyists. Scorpion carcasses were obtained through either the natural death of the animal or mortality through freezing. We collected two categories of taphonomic data on scorpion molts and carcasses: 1) the initial post-mortem (for carcasses) or postmolt (for exuvia) exoskeletal posture and 2) the order and timing of disarticulation of the exoskeleton (i.e., the disarticulation sequence) through subsequent tumbling experiments.
Death/molt posture.--Intact scorpion carcasses and exuvia were photographed, and the following exoskeletal characteristics were recorded for each specimen: 1) curvature of the mesosoma and metasoma; 2) presence or absence of telescoped mesosomal and metasomal segments; 3) position/orientation of the chelicerae; 4) position/orientation of the walking legs; and 5) position/orientation of the pedipalps. A total of 13 carcasses and 13 molts were used in this study. Twenty-four fossil scorpions from the collections of the Yale Peabody Museum (YPM) were photographed and described following the same five criteria.
Tumbling.--After documenting the initial condition of the exoskeleton, scorpions were treated in one of three ways: 1) tumbling (wet)-13 carcasses and 11 exuvia were tumbled to the point of complete disarticulation in fresh water inoculated by the addition of water from an aquarium; 2) tumbling (dry)--one carcass and two exuvia were tumbled dry until disarticulated; 3) one carcass and one exuvium were left to decay in inoculated freshwater with no agitation as controls. Wet tumbling was done in one of two small (5-cm radius) plastic rock-tumblers available from hobby stores. One tumbler barrel had a smooth interior; the other tumbler had molded invaginations of the barrel wall that acted as interior bails. Dry tumbling of larger specimens was done in a larger (20-cm radius) tumbler with two internal bails. The tumblers were checked daily and the extent of disarticulation of the specimens recorded. Carcasses were kept frozen until used in the tumbling experiments to minimize potential differences in disarticulation between specimens due to differences in the degree of decay (Allison 1986).
Statistics.--Standard chi-square tests of independence with Yates correction (Preacher 2001) were used to compare the frequency of each of the five exoskeletal characteristics of death/molt postures listed above. To adjust for multiple tests, we modified the standard alpha level of 0.05 as per the conservative Bonferroni correction by dividing by 5 (the number of characteristics tested), so that P-values less than 0.01 were considered statistically significant (Preacher 2001). The chi-square calculations were carried out on an online calculator (Preacher 2001).
We used t-tests to compare the mean time-to-separation of various exoskeletal elements: pedipalp claws, pedipalp appendages (tibia and brachium), distal leg segments, proximal leg segments, last three metasomal segments, second metasomal segment, first metasomal segment, chelicerae, carapace, and total mesosomal separation. Two variables were considered: specimen type (molt or carcass) and tumbler type (smooth interior/bails). P-values less than 0.05 were considered significant. The sequence of disarticulation suggested by the mean time-to-separation of each exoskeletal element was also tested using 95% confidence intervals.
[FIGURES 1-2 OMITTED]
[FIGURES 3-4 OMITTED]
The t-tests and 95% confidence intervals were generated using SAS software, version 9.2 of the SAS System for Windows (SAS Institute Inc., Cary, NC, USA).
Taphonomic patterns, I. Death/molt posture.--The scorpion carcasses examined for this study exhibited the following characters: 1) retracted chelicerae (100% of the specimens); 2) straight body line (in dorsal view) with the metasoma extended straight back (100%); 3) pedipalps pulled in toward the prosoma (54%); and 4) walking legs folded against the body (77%) (Table 1 and Figures 7-18). In contrast, molts were characterized by the following features: 1) extended chelicerae (92%); 2) curved body line and curved metasoma (62%); 3) pedipalps pulled well back from the prosoma in an extended position (85%); and 4) splayed walking legs (100%) (Table 1 and Figures 7-18). Four of 13 molts (31 %) exhibited telescoped mesosomal segments and overlap of the ventral surface on the dorsomedial surface (Figures 11, 15). These observations held across the six different scorpion genera examined for this study, suggesting taxonomic independence of these body-posture criteria. The low P-values obtained in the chi-squared test (Table 1) indicate that our sample size is sufficiently large to reflect a significant difference (P < 0.05) between scorpion death and molt postures.
Taphonomic pattens, II. Disarticulation.--Previous actuotaphonomic studies on tumbling segmented, exoskeleton-bearing invertebrates suggested that freezing the animals does not affect the exoskeletal disarticulation sequence (Kidwell & Baumiller 1990 on echinoids). We detected no differences in disarticulation between scorpions that had been frozen versus scorpions that had died naturally. Time-to-total disarticulation of the specimens is given in Table 2.
Wet vs. Dry: Both exuvia and carcasses released complete, intact tergites under wet tumbling conditions. These elements were not broken by subsequent tumbling (tumbling was terminated with the dissociation of the last exoskeletal elements). Carcasses tumbled dry behaved as carcasses tumbled wet. However, molts tumbled dry were quickly (2-3 days) reduced to ragged-edged, broken exoskeletal pieces rather than separated, unbroken tergites.
Disarticulation Sequence: A disarticulation sequence comprises two components: order and timing. Order refers to the sequence in which a given exoskeletal element separates in relation to the other exoskeletal elements. For example, "legs, pedipalps, chelicerae" is a different disarticulation order than "pedipalps, legs, chelicerae." Timing refers to the elapsed time before an exoskeletal element separates. Only differences in order are noticeable in fossils, but a difference in order necessarily requires a difference in timing.
[FIGURES 5-6 OMITTED]
Molts and carcasses showed no significant differences in mean time to separation in any of the exoskeletal elements (Table 3, Row 1), indicating that there is no significant difference in the sequence or order of disarticulation for scorpion molts as compared to scorpion carcasses. Plots of 95% confidence intervals of the mean time to separation for each exoskeletal element (Figures 1-6) show a general pattern shared by molts and carcasses. The appendages (PC, PA, DL, PL, Ch in Figures 1-6) and metasoma (M345, M2, M1 in Figures 1-6) tend to separate from the rest of the body before the mesosoma disarticulates (TMS in Figures 1-6). For example, in Figure 6, the pedipalps separate on day 6, and the mesosoma disarticulates on day 12.
Using the rock-tumbler with the internal bails shortened disarticulation time for both molts (compare Figures 1 and 2) and carcasses (compare Figures 3 and 4). This tumbler effect is also reflected in the statistically significant values in Table 3, Row 2. However, the tumbler effect does not result in a statistically significant difference in disarticulation timing between molts and carcasses, as shown by the overlapping confidence intervals (compare Figure 1 with Figure 3 and Figure 2 with Figure 4).
A somewhat unexpected result was the comparison of times to total disarticulation. Molts proved to be as durable as carcasses when tumbled in water, as evidenced by the fact that the mean time to total disarticulation (see Table 3, Row 1, Column TMS, and Figures 5, 6) is not significantly different between molts and carcasses.
To summarize the statistical analysis of the tumbling data, molts and carcasses generally release appendages and metasomal segments early, the mesosoma is the most resilient exoskeletal unit for both exuvia and carcasses, and molts take as long as carcasses to reach total disarticulation.
DISCUSSION AND APPLICATION TO FOSSIL SCORPIONS
Scorpion molting and exuvia taphonomy.--Observations on ecdysis in modern scorpions support the criteria defined here of appendage position and body posture as diagnostic for distinguishing carcasses and exuvia. De Armas (1986) concluded that the position of the legs on a suitable substrate is critical for scorpions to successfully complete the process of ecdysis, and Gaban & Farley (2002) noted that the walking legs become rigid and fixed in place before ecdysis begins. These observations suggest that ecdysial leg position may be retained after ecdysis, although Gaban & Farley (2002) also observed that Paruroctonus mesaensis (Stahnke 1957) pulls its appendages medially during ecdysis. The exuvia of all the scorpion genera examined in our study show the splayed walking leg posture.
[FIGURES 7-18 OMITTED]
The position of the pedipalps differs between the exuvia and carcasses examined for this study. Our observations compliment those of Gaban & Farley (2002), who noted that Androctonus australis (Linnaeus 1758) holds its pedipalps in a distinctive position before ecdysis, with the chelae sharply angled toward each other. These authors noted that this pre-molt posture contrasts with the posture of scorpions at rest, in which the pedipalps are retracted. More than half of the carcasses examined in this study retained their pedipalps in a retracted position, suggesting that the relaxed position also served as a post-mortem posture.
Observations on modern scorpions also support body line as a criterion for distinguishing exuvia (curved) from carcasses (straight). Gaban & Farley (2002) cite examples of exuvia of A. australis, P. mesaenis, and Parabuthus transvaalicus Purcell 1899 that are curved dorsally or to one side.
Fossil scorpion taphonomy.--We examined 24 well-preserved, nearly complete fossil scorpions from the Ciurca collection at the Yale Peabody Museum (YPM; Table 4) and applied our taphonomic criteria in an attempt to characterize each specimen as molt or carcass. One or more of the four distinguishing criteria (body line, position of chelicerae, position of walking legs, and position of pedipalps) could be identified in 85-90% of the YPM specimens (Table 4). Approximately 89% of the classifiable YPM specimens fit the criteria for molts (Table 4). The results of the YMP census support the conclusion of other authors that the bulk of the scorpion fossil record comprises exuvia (Kjellesvig-Waering 1986).
Most authors of papers on scorpion systematics do not include taphonomic data in their description of new specimens, nor do they make a determination of whether their illustrated specimens represent molts or carcasses. The taphonomic criteria developed herein can also be used to make the molt/carcass determination for fossil scorpions illustrated in the literature (Table 5).
The results of the tumbling experiments suggested that scorpion molts in water are nearly as durable as scorpion carcasses, as measured by time to total disarticulation (Tables 2, 3). This observation is interesting because it runs counter to the intuitive conclusion that molts must be more fragile than carcasses, and it calls into question the assumption that intact fossil scorpions are more likely the remains of the more "robust" carcass than the presumably "fragile" exuvium (Wills 1959; Jeram 2001; Gaban & Farley 2002).
The scorpion body plan is strikingly similar to that of the extinct eurypterids (Chelicerata: Eurypterida), and on this basis, scorpions can be considered reasonable taphonomic analogues for their extinct chelicerate cousins. Therefore, the criteria for distinguishing fossil scorpion molts and carcasses may also be useful for distinguishing fossil eurypterid molts and carcasses. A recent study of eurypterid molting (Tetlie et al. 2008) concluded that eurypterids indeed molted in much the same manner as modern scorpions, in spite of the obvious ecological differences between the aquatic eurypterids and the terrestrial scorpions.
We would like to thank Derek Briggs and Erik Tetlie for their discussions and collaboration and Mary Marazita for help with the statistical analyses. Many thanks also to Kevin Cash, Matt Wilhm, Matt Grahm, and Mike Weissman for their donation of scorpion molts and carcasses, and Tomasz Baumiller for the use of his tumbling apparatus. The paper was improved by the constructive comments of Derek Briggs, Robert Anstey, and two anonymous reviewers. Funding in support of this project was provided by the Schuchert Fund of the Yale Peabody Museum, the North-Central Section of the Geological Society of America, the College of Natural Science, the Department of Geological Sciences, and the Honors College at Michigan State University.
Manuscript received 30 January 2009, revised 23 July 2009.
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Victoria E. McCoy and Danita S. Brandt (1): Department of Geological Sciences, Michigan State University, 206 Natural Science Building, East Lansing, Michigan 48824, USA
(1) Corresponding author. E-mail: email@example.com
Table 1.--Taphonomic characteristics of scorpion molts and carcasses. Significant p-values are in bold. 1This cell does not total 13 because six exuvia lack appendages. 2Chi-square with Yates correction, all one degree of freedom. Character Description Molt (n = 13) Carcass (n = 13) Chelicerae Extended 12 0 Retracted 1 13 Pedipalps Extended 11 6 Retracted 2 7 Body line Curved 8 0 Straight 5 13 Walking legs Splayed 71 3 Folded 0 10 Telescoping Present 4 0 of segments Absent 9 13 [Chi- Character Description square.sup.2] P Chelicerae Extended 18.73 1.5 x [10.sup.-5] Retracted Pedipalps Extended 2.71 0.10 Retracted Body line Curved 8.85 0.003 Straight Walking legs Splayed 7.91 0.005 Folded Telescoping Present 2.66 0.10 of segments Absent Table 2.--Laboratory treatment of scorpion carcasses and molts. Molt/ Species Carcass Wet/Dry Tumbler Pandinus imperator (C.L. Koch 1841) molt dry bail-lg Leiurus quinquestriatus (Ehrenberg 1928) molt dry smooth P. imperator molt wet smooth P. imperator molt wet smooth Parabuthus transvaalicus molt wet smooth P. transvaalicus molt wet smooth P. imperator molt wet smooth P. imperator molt wet smooth P. imperator molt wet bail P. imperator (juv) molt wet smooth P. imperator molt wet smooth P. imperator molt wet bail P. imperator (juv) molt wet smooth P. imperator (juv) carcass dry bail-lg P. imperator (juv) carcass wet smooth Anuroctonus phaiodactylus (Wood 1863) carcass wet smooth Smeringurus mesaensis (Stanhke 1957) carcass wet smooth S.mesaensis carcass wet bail S.mesaensis carcass wet smooth S.mesaensis carcass wet bail S.mesaensis (juv) carcass wet bail S.mesaensis carcass wet smooth S.mesaensis carcass wet bail S.mesaensis carcass wet smooth S.mesaensis (juv) carcass wet bail S.mesaensis (juv) carcass wet smooth Vaejovis spinigerus (Wood 1863) carcass wet smooth Species Time (days) Pandinus imperator (C.L. Koch 1841) 2 Leiurus quinquestriatus (Ehrenberg 1928) 16 P. imperator 14 P. imperator 7 Parabuthus transvaalicus 15 P. transvaalicus 11 P. imperator 18 P. imperator 12 P. imperator 18 P. imperator (juv) 10 P. imperator 11 P. imperator 6 P. imperator (juv) 7 P. imperator (juv) 4 P. imperator (juv) 22 Anuroctonus phaiodactylus (Wood 1863) 8 Smeringurus mesaensis (Stanhke 1957) 19 S.mesaensis 18 S.mesaensis 11 S.mesaensis 10 S.mesaensis (juv) 6 S.mesaensis 13 S.mesaensis 10 S.mesaensis 11 S.mesaensis (juv) 3 S.mesaensis (juv) 13 Vaejovis spinigerus (Wood 1863) 12 Table 3.--Comparison of molt-carcass and tumbler effects on disarticulation. P-values from the t-tests on the mean time to separation of exoskeletal tergites; significant P-values are in bold. S = smooth tumbler, B = tumbler with bails, PC = pedipalp claws, PA = pedipalp appendages, DL = distal leg segments, PL = proximal leg segments, M345 = third, fourth and fifth metasomal segments as one unit, M2 = second metasomal segment, M1 = first metasomal segment, Ch = chelicerae, Ca = carapace, and TMS = total mesosomal separation (= total exoskeletal disarticulation). The lack of significant P-values in the first row indicates that there are no differences in the timing of disarticulation between molts and carcasses. In the second row, the majority of the P- values are significant, reflecting differences in the timing of disarticulation between specimens in the smooth tumbler and specimens in the tumbler with the bail. PC PA DL PL M345 molt vs carcass 0.6817 0.7332 0.9333 0.9858 0.65 S- vs. B-tumbler 0.0001 0.0001 0.0083 0.0085 0.005 M2 M1 Ch Ca TMS molt vs carcass 0.932 0.605 0.4175 0.363 0.891 S- vs. B-tumbler 0.0025 0.939 0.0053 0.089 0.255 Table 4.--YPM specimens and identification as molt or carcass based on the criteria defined herein; 'Vindicates presence, "-" denotes missing features or that determination could not be made, "?" denotes identification could not be determined due to poor preservation. E = extended, R = retracted, C = curved, St = straight, Sp = splayed, F = folded, P = present, A = absent. In the age column, MP = Middle Pennsylvanian, LS = Late Silurian. Specimen # Chelicerae Pedipalps Taxon E R E R typical carcass - + - + typical molt + - + - YPM 126 Anthracoscorpio? sp. - - - - YPM 206691 'Archaeophonus + - + - eurypteroides' YPM 00128 Eoscorpius + - + - carbonarius YPM 139 E. carbonarius - - - - YPM 138 E. danielsi - - + - YPM 212155 Mazonia woodiana + - + - YPM 127 Palaeobuthus - - - - distinctus YPM 212157 P. distinctus - - - - YPM 140 Palaeopisthacanthus + - + - schucherti YPM 130 Proscorpius + - + - distinctus YPM 133 P. distinctus - - + - YPM 208121 P. osborni - - + - YPM 208125 P. osborni + - + - YPM 208126 P. osborni - - + - YPM 208127 P. osborni - - - - YPM 208129 P. osborni - + - + YPM 208130 P. osborni + - + - YPM 208131 P. osborni - - + - YPM 209823 P. osborni + - + - YPM 212926 P. osborni - - + - YPM 212927 P. osborni - - - - YPM 212928 P. osborni - - - - YPM 206692 'Stoermeroscorpio - - + - delicatus' Specimen # Body Line Walking legs Telescoping ID C St Sp F P A typical carcass - + - + - + carcass typical molt + - + - + - molt YPM 126 - + - - - + ? YPM 206691 - + + - - - molt YPM 00128 - + + - - - molt YPM 139 - - - - - - ? YPM 138 - - + - - - molt YPM 212155 - + - - - - molt YPM 127 - + - - - - ? YPM 212157 + - - - - - molt YPM 140 - - - - - - molt YPM 130 - + + - - - molt YPM 133 + - - - - - molt YPM 208121 + - + - + - molt YPM 208125 - + + - - + molt YPM 208126 + - + - - - molt YPM 208127 - + - - + - ? YPM 208129 - + - + - + carcass YPM 208130 + - + - - - molt YPM 208131 - + - - - + carcass YPM 209823 + - + - - - molt YPM 212926 - + + - - - molt YPM 212927 - + - - - - ? YPM 212928 - - - - - - ? YPM 206692 + - + - - - molt Specimen # Locality Age Formation typical carcass typical molt YPM 126 Grundy Co., MP Carbondale IL YPM 206691 Herkimer, LS Willimsville NY YPM 00128 Grundy Co., MP Carbondale IL YPM 139 Grundy Co., MP Carbondale IL YPM 138 Grundy Co., MP Carbondale IL YPM 212155 Welland, LS Fiddler's ON Green YPM 127 Grundy Co., MP Carbondale IL YPM 212157 Grundy Co., MP Carbondale IL YPM 140 Grundy Co., MP Carbondale IL YPM 130 Grundy Co., MP Carbondale IL YPM 133 Grundy Co., MP Carbondale IL YPM 208121 Herkimer, NY LS Williamsville YPM 208125 Herkimer, NY LS Williamsville YPM 208126 Herkimer, NY LS Williamsville YPM 208127 Herkimer, NY LS Fiddler's Green YPM 208129 Herkimer, NY LS Williamsville YPM 208130 Herkimer, NY LS Williamsville YPM 208131 Herkimer, NY LS Williamsville YPM 209823 Herkimer, NY LS Williamsville YPM 212926 Herkimer, NY LS Fiddler's Green YPM 212927 Herkimer, NY LS Fiddler's Green YPM 212928 Herkimer, NY LS Fiddler's Green YPM 206692 Herkimer, NY LS Williamsville Table 5.--Literature survey with identification of illustrated specimens as molt or carcass based on the criteria defined herein; "+" indicates presence, "-" denotes missing features or poor preservation. E = extended, R = retracted, C = curved, St = straight, Sp = splayed, F = folded, P = present, A = absent. Chelicerae Pedipalps Body Line Author Figure E R E R C St typical carcass - + - + - + typical molt + - + - + - Carvalho & Lourenco 2001 Figure 2 - + + - - + Lourenco & Gall 2004 - - + - - + Santiago-Blay 1988 Figure 1-2 - - + - + - Santiago-Blay et al. 2004 Figure 1 - + - - - + Walking legs Telescoping Author Sp F P A Identification typical carcass - + - + carcass typical molt + - + - molt Carvalho & Lourenco 2001 - + - - carcass Lourenco & Gall 2004 - + - - molt Santiago-Blay 1988 + - - - molt Santiago-Blay et al. 2004 - - - - carcass
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