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Big guns of the Cambrian Explosion : Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia. / Sarsembaev, Z. A.; Marusin, V. V.

в: Estudios Geologicos, Том 75, № 2, 2019.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Sarsembaev, ZA & Marusin, VV 2019, 'Big guns of the Cambrian Explosion: Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia', Estudios Geologicos, Том. 75, № 2. https://doi.org/10.3989/egeol.43595.568

APA

Sarsembaev, Z. A., & Marusin, V. V. (2019). Big guns of the Cambrian Explosion: Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia. Estudios Geologicos, 75(2). https://doi.org/10.3989/egeol.43595.568

Vancouver

Sarsembaev ZA, Marusin VV. Big guns of the Cambrian Explosion: Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia. Estudios Geologicos. 2019;75(2). doi: 10.3989/egeol.43595.568

Author

Sarsembaev, Z. A. ; Marusin, V. V. / Big guns of the Cambrian Explosion : Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia. в: Estudios Geologicos. 2019 ; Том 75, № 2.

BibTeX

@article{64674e41a6a24969ba8f1e6fa7837b61,
title = "Big guns of the Cambrian Explosion: Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia",
abstract = "The basal Cambrian Stage 2 strata of the Olenek Uplift host diverse assemblages of macroscopic fossils, which closely resemble certain small skeletal taxa early reported from this section and typical for the Terreneuvian Epoch. Herein studied macroscopic assemblage includes helcionellid, stenothecid and kharkhaniid molluscs, and anabaritids and circothecid hyoliths. Among the assemblage, only anabaritids and some citrcothecid hyoliths exhibit relics of calcite shell, whereas most of the fossils reveal no evidence of rigid biomineralized exoskeleton. Hence, at least these problematic Cambrian organisms had reached macroscopic sizes (up to 35 mm long) and were covered with calcite shells at the very beginning of the Cambrian Age 2.",
keywords = "Biomineralization, Cambrian, Cambrian explosion, Siberian Platform, MOLLUSKS",
author = "Sarsembaev, {Z. A.} and Marusin, {V. V.}",
year = "2019",
doi = "10.3989/egeol.43595.568",
language = "English",
volume = "75",
journal = "Estudios Geologicos",
issn = "0367-0449",
publisher = "CSIC Consejo Superior de Investigaciones Cientificas",
number = "2",

}

RIS

TY - JOUR

T1 - Big guns of the Cambrian Explosion

T2 - Macroskeletal benthic assemblage in the lower Cambrian Stage 2 of the Olenek Uplift, Arctic Siberia

AU - Sarsembaev, Z. A.

AU - Marusin, V. V.

PY - 2019

Y1 - 2019

N2 - The basal Cambrian Stage 2 strata of the Olenek Uplift host diverse assemblages of macroscopic fossils, which closely resemble certain small skeletal taxa early reported from this section and typical for the Terreneuvian Epoch. Herein studied macroscopic assemblage includes helcionellid, stenothecid and kharkhaniid molluscs, and anabaritids and circothecid hyoliths. Among the assemblage, only anabaritids and some citrcothecid hyoliths exhibit relics of calcite shell, whereas most of the fossils reveal no evidence of rigid biomineralized exoskeleton. Hence, at least these problematic Cambrian organisms had reached macroscopic sizes (up to 35 mm long) and were covered with calcite shells at the very beginning of the Cambrian Age 2.

AB - The basal Cambrian Stage 2 strata of the Olenek Uplift host diverse assemblages of macroscopic fossils, which closely resemble certain small skeletal taxa early reported from this section and typical for the Terreneuvian Epoch. Herein studied macroscopic assemblage includes helcionellid, stenothecid and kharkhaniid molluscs, and anabaritids and circothecid hyoliths. Among the assemblage, only anabaritids and some citrcothecid hyoliths exhibit relics of calcite shell, whereas most of the fossils reveal no evidence of rigid biomineralized exoskeleton. Hence, at least these problematic Cambrian organisms had reached macroscopic sizes (up to 35 mm long) and were covered with calcite shells at the very beginning of the Cambrian Age 2.

KW - Biomineralization

KW - Cambrian

KW - Cambrian explosion

KW - Siberian Platform

KW - MOLLUSKS

UR - http://www.scopus.com/inward/record.url?scp=85075979880&partnerID=8YFLogxK

U2 - 10.3989/egeol.43595.568

DO - 10.3989/egeol.43595.568

M3 - Article

AN - SCOPUS:85075979880

VL - 75

JO - Estudios Geologicos

JF - Estudios Geologicos

SN - 0367-0449

IS - 2

ER -

ID: 22575016