Traces of Locomotion of Ediacaran Macroorganisms

We describe traces of macroorganisms in association with the body imprints of trace-producers from Ediacaran (Vendian) deposits of the southeastern White Sea region. They are interpreted as traces of locomotion and are not directly related to a food gathering. The complex remains belong to three spe...

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Published in:Geosciences
Main Authors: Andrey Ivantsov, Aleksey Nagovitsyn, Maria Zakrevskaya
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/geosciences9090395
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spelling ftmdpi:oai:mdpi.com:/2076-3263/9/9/395/ 2023-08-20T04:10:19+02:00 Traces of Locomotion of Ediacaran Macroorganisms Andrey Ivantsov Aleksey Nagovitsyn Maria Zakrevskaya agris 2019-09-11 application/pdf https://doi.org/10.3390/geosciences9090395 EN eng Multidisciplinary Digital Publishing Institute Biogeosciences https://dx.doi.org/10.3390/geosciences9090395 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 9; Issue 9; Pages: 395 Ediacaran biota trace fossils Dickinsonia Kimberella Tribrachidium Text 2019 ftmdpi https://doi.org/10.3390/geosciences9090395 2023-07-31T22:35:55Z We describe traces of macroorganisms in association with the body imprints of trace-producers from Ediacaran (Vendian) deposits of the southeastern White Sea region. They are interpreted as traces of locomotion and are not directly related to a food gathering. The complex remains belong to three species: Kimberella quadrata, Dickinsonia cf. menneri, and Tribrachidium heraldicum. They were found in three different burials. The traces have the form of narrow ridges or wide bands (grooves and linear depressions on natural imprints). In elongated Kimberella and Dickinsonia, the traces are stretched parallel to the longitudinal axis of the body and extend from its posterior end. In the case of the isometric Tribrachidium, the trace is directed away from the margin of the shield. A short length of the traces indicates that they were left by the organisms that were covered with the sediment just before their death. The traces overlaid the microbial mat with no clear signs of deformation under or around the traces. A trace substance, apparently, differed from the material of the bearing layers (i.e., a fine-grained sandstone or siltstone) and was not preserved on the imprints. This suggests that the traces were made with organic material, probably mucus, which was secreted by animals in a stressful situation. The mucus traced the movements of the organism before death. The discovered traces of locomotion are direct evidence of the ability of some Ediacaran macroorganisms to move independently. Text White Sea MDPI Open Access Publishing White Sea Geosciences 9 9 395
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Ediacaran biota
trace fossils
Dickinsonia
Kimberella
Tribrachidium
spellingShingle Ediacaran biota
trace fossils
Dickinsonia
Kimberella
Tribrachidium
Andrey Ivantsov
Aleksey Nagovitsyn
Maria Zakrevskaya
Traces of Locomotion of Ediacaran Macroorganisms
topic_facet Ediacaran biota
trace fossils
Dickinsonia
Kimberella
Tribrachidium
description We describe traces of macroorganisms in association with the body imprints of trace-producers from Ediacaran (Vendian) deposits of the southeastern White Sea region. They are interpreted as traces of locomotion and are not directly related to a food gathering. The complex remains belong to three species: Kimberella quadrata, Dickinsonia cf. menneri, and Tribrachidium heraldicum. They were found in three different burials. The traces have the form of narrow ridges or wide bands (grooves and linear depressions on natural imprints). In elongated Kimberella and Dickinsonia, the traces are stretched parallel to the longitudinal axis of the body and extend from its posterior end. In the case of the isometric Tribrachidium, the trace is directed away from the margin of the shield. A short length of the traces indicates that they were left by the organisms that were covered with the sediment just before their death. The traces overlaid the microbial mat with no clear signs of deformation under or around the traces. A trace substance, apparently, differed from the material of the bearing layers (i.e., a fine-grained sandstone or siltstone) and was not preserved on the imprints. This suggests that the traces were made with organic material, probably mucus, which was secreted by animals in a stressful situation. The mucus traced the movements of the organism before death. The discovered traces of locomotion are direct evidence of the ability of some Ediacaran macroorganisms to move independently.
format Text
author Andrey Ivantsov
Aleksey Nagovitsyn
Maria Zakrevskaya
author_facet Andrey Ivantsov
Aleksey Nagovitsyn
Maria Zakrevskaya
author_sort Andrey Ivantsov
title Traces of Locomotion of Ediacaran Macroorganisms
title_short Traces of Locomotion of Ediacaran Macroorganisms
title_full Traces of Locomotion of Ediacaran Macroorganisms
title_fullStr Traces of Locomotion of Ediacaran Macroorganisms
title_full_unstemmed Traces of Locomotion of Ediacaran Macroorganisms
title_sort traces of locomotion of ediacaran macroorganisms
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/geosciences9090395
op_coverage agris
geographic White Sea
geographic_facet White Sea
genre White Sea
genre_facet White Sea
op_source Geosciences; Volume 9; Issue 9; Pages: 395
op_relation Biogeosciences
https://dx.doi.org/10.3390/geosciences9090395
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/geosciences9090395
container_title Geosciences
container_volume 9
container_issue 9
container_start_page 395
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