A Unique Winged Euthycarcinoid from the Permian of Antarctica
Euthycarcinoid arthropods (Cambrian—Triassic) were likely the first animals to transition from oceanic to freshwater and emergent environments. Although their basic bauplan is well known, they have a poor fossil record because their non-sclerotized exoskeleton was rarely preserved. Euthycarcinoids...
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ftbioone:10.1017/jpa.2017.28 2024-06-02T07:57:25+00:00 A Unique Winged Euthycarcinoid from the Permian of Antarctica Joseph H. Collette John L. Isbell Molly F. Miller Joseph H. Collette John L. Isbell Molly F. Miller world 2017-09-01 text/HTML https://doi.org/10.1017/jpa.2017.28 en eng The Paleontological Society doi:10.1017/jpa.2017.28 All rights reserved. https://doi.org/10.1017/jpa.2017.28 Text 2017 ftbioone https://doi.org/10.1017/jpa.2017.28 2024-05-07T00:47:45Z Euthycarcinoid arthropods (Cambrian—Triassic) were likely the first animals to transition from oceanic to freshwater and emergent environments. Although their basic bauplan is well known, they have a poor fossil record because their non-sclerotized exoskeleton was rarely preserved. Euthycarcinoids' unusual morphology (varying numbers of body segments, seemingly dichotomous possession of either mandibles or a labrum, specialized or generalized limbs, and possession by some euthycarcinoid species of sternal pores—structures possibly analogous to coxal vesicles in myriapods) contribute to uncertainty regarding their relationship to other arthropod groups; while their poor fossil record masks the evolutionary transitions within and between the separate realms they inhabited (marine, freshwater, emergent). A new euthycarcinoid from a Permian polar proglacial lake is described herein that is morphologically unlike all other euthycarcinoids, and interpreted as being well adapted for a nekton-benthic lifestyle. Antarcticarcinus pagoda n. gen. n. sp. possesses a pair of large wing-like processes that project laterally from the preabdominal dorsal exoskeleton. A trace fossil from the overlying Mackellar Formation, cf. Orbiculichnus, which was previously interpreted as having been produced by insects taking off or landing on wet sediments, is reinterpreted herein as being produced by A. pagoda n. gen. n. sp. due to the high degree of morphological similarity between traces and body fossils. This occurrence indicates that euthycarcinoids were able to adapt to life in temperate freshwater environments, while possible subaerial adaptations hint at an ability to breathe air. Indeed, if euthycarcinoids could breathe air, Cambrian terrestrial forays and rapid transition (by the Ordovician) into freshwater environments might be explained. Text Antarc* Antarctica BioOne Online Journals Mackellar ENVELOPE(-58.455,-58.455,-62.079,-62.079) Journal of Paleontology 91 5 987 993 |
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BioOne Online Journals |
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ftbioone |
language |
English |
description |
Euthycarcinoid arthropods (Cambrian—Triassic) were likely the first animals to transition from oceanic to freshwater and emergent environments. Although their basic bauplan is well known, they have a poor fossil record because their non-sclerotized exoskeleton was rarely preserved. Euthycarcinoids' unusual morphology (varying numbers of body segments, seemingly dichotomous possession of either mandibles or a labrum, specialized or generalized limbs, and possession by some euthycarcinoid species of sternal pores—structures possibly analogous to coxal vesicles in myriapods) contribute to uncertainty regarding their relationship to other arthropod groups; while their poor fossil record masks the evolutionary transitions within and between the separate realms they inhabited (marine, freshwater, emergent). A new euthycarcinoid from a Permian polar proglacial lake is described herein that is morphologically unlike all other euthycarcinoids, and interpreted as being well adapted for a nekton-benthic lifestyle. Antarcticarcinus pagoda n. gen. n. sp. possesses a pair of large wing-like processes that project laterally from the preabdominal dorsal exoskeleton. A trace fossil from the overlying Mackellar Formation, cf. Orbiculichnus, which was previously interpreted as having been produced by insects taking off or landing on wet sediments, is reinterpreted herein as being produced by A. pagoda n. gen. n. sp. due to the high degree of morphological similarity between traces and body fossils. This occurrence indicates that euthycarcinoids were able to adapt to life in temperate freshwater environments, while possible subaerial adaptations hint at an ability to breathe air. Indeed, if euthycarcinoids could breathe air, Cambrian terrestrial forays and rapid transition (by the Ordovician) into freshwater environments might be explained. |
author2 |
Joseph H. Collette John L. Isbell Molly F. Miller |
format |
Text |
author |
Joseph H. Collette John L. Isbell Molly F. Miller |
spellingShingle |
Joseph H. Collette John L. Isbell Molly F. Miller A Unique Winged Euthycarcinoid from the Permian of Antarctica |
author_facet |
Joseph H. Collette John L. Isbell Molly F. Miller |
author_sort |
Joseph H. Collette |
title |
A Unique Winged Euthycarcinoid from the Permian of Antarctica |
title_short |
A Unique Winged Euthycarcinoid from the Permian of Antarctica |
title_full |
A Unique Winged Euthycarcinoid from the Permian of Antarctica |
title_fullStr |
A Unique Winged Euthycarcinoid from the Permian of Antarctica |
title_full_unstemmed |
A Unique Winged Euthycarcinoid from the Permian of Antarctica |
title_sort |
unique winged euthycarcinoid from the permian of antarctica |
publisher |
The Paleontological Society |
publishDate |
2017 |
url |
https://doi.org/10.1017/jpa.2017.28 |
op_coverage |
world |
long_lat |
ENVELOPE(-58.455,-58.455,-62.079,-62.079) |
geographic |
Mackellar |
geographic_facet |
Mackellar |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
https://doi.org/10.1017/jpa.2017.28 |
op_relation |
doi:10.1017/jpa.2017.28 |
op_rights |
All rights reserved. |
op_doi |
https://doi.org/10.1017/jpa.2017.28 |
container_title |
Journal of Paleontology |
container_volume |
91 |
container_issue |
5 |
container_start_page |
987 |
op_container_end_page |
993 |
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1800740570695467008 |