The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia

The fragments of osteostracan exoskeleton from the Lover Devonian Severnaya Zemlya Formation of the Severnaya Zemlya archipelago, viz., Ungulaspis arctoa AFANASSIEVA & KARATAJUTE-TALIMAA, 1998 and Ateleaspis sp., were studied. The structure of the exoskeleton of non-tremataspid osteostracans was...

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Main Author: Afanassieva, Olga B.
Format: Article in Journal/Newspaper
Language:English
Published: Faculty of Geology University of Warsaw 2003
Subjects:
Online Access:https://gq.pgi.gov.pl/agp/article/view/10328
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spelling ftjgq:oai:geojournals.pgi.gov.pl:article/10328 2024-09-15T17:50:01+00:00 The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia Afanassieva, Olga B. 2003-06-01 application/pdf https://gq.pgi.gov.pl/agp/article/view/10328 eng eng Faculty of Geology University of Warsaw https://gq.pgi.gov.pl/agp/article/view/10328/8840 https://gq.pgi.gov.pl/agp/article/view/10328 Acta Geologica Polonica; Vol. 49 No. 2 (1999): Circum-Arctic Palaeozoic Vertebrates; 119-123 Acta Geologica Polonica; Tom 49 Nr 2 (1999): Circum-Arctic Palaeozoic Vertebrates; 119-123 Osteostraci Agnatha Lower Devonian Severnaya Zemlya info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2003 ftjgq 2024-07-30T03:29:09Z The fragments of osteostracan exoskeleton from the Lover Devonian Severnaya Zemlya Formation of the Severnaya Zemlya archipelago, viz., Ungulaspis arctoa AFANASSIEVA & KARATAJUTE-TALIMAA, 1998 and Ateleaspis sp., were studied. The structure of the exoskeleton of non-tremataspid osteostracans was investigated by SEM for the first time. A reconstruction of the structure of the Ungulaspis arctoa exoskeleton is suggested. Because of the poorer preservation of the Ateleaspis sp., only preliminary observations on the thin structure of its exoskeleton could be made. The forms under investigation are characterized by a similar type of sculpture on the surface of the shied (small tubercles) and on the body scales (thin crests). Some similarities in the structure of their shield exoskeleton (the presence of distinctly expressed tesserae, the presence of radiating canals, the probable absence of perforated septa and pore fields) were indicated. Ungulaspis arctoa is remarkable in the possessing macromorphological features typical of both the Ateleaspis- and Scolenaspis-like osteostracans. This similarity in the structure of exoskeleton of the investigated forms provides additional evidence in support of the affinity of these groups of osteostracans and their possible origin from common ancestors. Article in Journal/Newspaper Arctic Severnaya Zemlya Geological Quarterly
institution Open Polar
collection Geological Quarterly
op_collection_id ftjgq
language English
topic Osteostraci
Agnatha
Lower Devonian
Severnaya Zemlya
spellingShingle Osteostraci
Agnatha
Lower Devonian
Severnaya Zemlya
Afanassieva, Olga B.
The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
topic_facet Osteostraci
Agnatha
Lower Devonian
Severnaya Zemlya
description The fragments of osteostracan exoskeleton from the Lover Devonian Severnaya Zemlya Formation of the Severnaya Zemlya archipelago, viz., Ungulaspis arctoa AFANASSIEVA & KARATAJUTE-TALIMAA, 1998 and Ateleaspis sp., were studied. The structure of the exoskeleton of non-tremataspid osteostracans was investigated by SEM for the first time. A reconstruction of the structure of the Ungulaspis arctoa exoskeleton is suggested. Because of the poorer preservation of the Ateleaspis sp., only preliminary observations on the thin structure of its exoskeleton could be made. The forms under investigation are characterized by a similar type of sculpture on the surface of the shied (small tubercles) and on the body scales (thin crests). Some similarities in the structure of their shield exoskeleton (the presence of distinctly expressed tesserae, the presence of radiating canals, the probable absence of perforated septa and pore fields) were indicated. Ungulaspis arctoa is remarkable in the possessing macromorphological features typical of both the Ateleaspis- and Scolenaspis-like osteostracans. This similarity in the structure of exoskeleton of the investigated forms provides additional evidence in support of the affinity of these groups of osteostracans and their possible origin from common ancestors.
format Article in Journal/Newspaper
author Afanassieva, Olga B.
author_facet Afanassieva, Olga B.
author_sort Afanassieva, Olga B.
title The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
title_short The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
title_full The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
title_fullStr The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
title_full_unstemmed The exoskeleton of Ungulaspis and Ateleaspis (Osteostraci, Agnatha) from the Lower Devonian of Severnaya Zemlya, Russia
title_sort exoskeleton of ungulaspis and ateleaspis (osteostraci, agnatha) from the lower devonian of severnaya zemlya, russia
publisher Faculty of Geology University of Warsaw
publishDate 2003
url https://gq.pgi.gov.pl/agp/article/view/10328
genre Arctic
Severnaya Zemlya
genre_facet Arctic
Severnaya Zemlya
op_source Acta Geologica Polonica; Vol. 49 No. 2 (1999): Circum-Arctic Palaeozoic Vertebrates; 119-123
Acta Geologica Polonica; Tom 49 Nr 2 (1999): Circum-Arctic Palaeozoic Vertebrates; 119-123
op_relation https://gq.pgi.gov.pl/agp/article/view/10328/8840
https://gq.pgi.gov.pl/agp/article/view/10328
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