NEOICHNOLOGY OF AMPHIBIOUS ARTHROPODS: EFFECTS OF SUBAQUEOUS AND SUBAERIAL SUBSTRATE CONDITIONS ON TRACE MORPHOLOGY
Author:
DEVINE L.K.1, MINTER N.J.1
Affiliation:
1. School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, PO1 3QL, UK
Abstract
Abstract
Neoichnology, the study of the traces of extant organisms, provides a vital tool for better understanding trace fossils. We conducted neoichnological experiments to test hypotheses regarding producers and the effects of substrate conditions on trace fossils produced by aquatic to amphibious arthropods. Our experiments comprised two protocols: subaerial and subaqueous substrates; and we utilized five arthropods: fully aquatic ostracods (Ostracoda indet.), to amphibious horseshoe crabs (Limulus polyphemus), shore crabs (Carcinus maenas), and scarlet hermit crabs (Paguristes cadenati), and the largely terrestrial sea slaters (Ligia oceanica). The different arthropods were observed performing locomotory, resting/stationary, and feeding behaviors, which all resulted in different traces influenced by the substrate conditions and their preference for living in and out of water. In general, trace depth increased with arthropod mass and, for each individual arthropod except the scarlet hermit crab, trace depth was also greater in subaerial compared to subaqueous substrates. In the majority of cases, comparisons with selected trace fossils supported previous hypotheses as to their producers. The traces of horseshoe crabs, shore crabs, sea slaters, and ostracods resembled the ichnotaxa Kouphichnium, Laterigradus, Pterichnus, and Mermia, respectively. Other experimental work has shown hermit crabs produce traces similar to Coenobichnus and our results further increase the range of trace morphologies that can be attributed to hermit crabs. The results of this research have bearing on debates in ichnology where the interpretation of producers and substrate conditions at the time of trace formation are critical, such as the trace fossil evidence for the colonization of land.
Publisher
Society for Sedimentary Geology
Subject
Paleontology,Ecology, Evolution, Behavior and Systematics
Reference54 articles.
1. Bengston,
S.
,
Rasmussen,B.,
Zi,J.,
Fletcher,I.,
Gehling,J., and
Runnegar,B.,
2021,
Eocene animal trace fossils in 1.7-billion-year-old metaquartzites: Proceedings of the National Academy of Sciences, v. 118, article number: e2105707118. 2. Bertling,
M.
,
Braddy,S.J.,
Bromley,R.G.,
Demathieu,G.R.,
Genise,J.,
Mikulás,R.,
Nielsen,J.K.,
Nielsen,K.S.S.,
Rindsberg,A.K.,
Schlirf,M., and
Uchman,A.,
2006,
Names for trace fossils: a uniform approach:
Lethaia,
v.39,
p.265–286. 3. Brand,
L.R.
,
1996,
Variations in salamander trackways resulting from substrate differences:
Journal of Paleontology,
v.70,
p.1004–1010. 4. Brewer,
E.
and
Falk,A.,
2021,
Neoichnology: why should we care about peck marks and dust baths?:
Ethology Ecology and Evolution,
v.33,
p.90–97. 5. Briggs,
D.
,
Wright,J., and
Suthren,R.,
2019,
COMMENT: Death near the shoreline, not life on land: Ordovician arthropod trackways in the Borrowdale Volcanic Group, UK:
Geology,
v.47,
p.e463–e464.
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|