Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard

A distinctive carbonate shallowing-upward sequence occurs within the Upper Riphean (750-800 Ma) Hunnberg Formation of Nordaustlandet, Svalbard. Clastic limestones deposited in an open coastal marine environment pass upward into columnar stromatolitic bioherms, and these, in turn, are overlain by fin...

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Main Author: Knoll, Andrew
Language:English
Published: The Paleontological Society 1984
Subjects:
Online Access:http://nrs.harvard.edu/urn-3:HUL.InstRepos:4554331
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spelling ftharvardudash:oai:dash.harvard.edu:1/4554331 2023-05-15T17:24:13+02:00 Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard Knoll, Andrew 1984 application/pdf http://nrs.harvard.edu/urn-3:HUL.InstRepos:4554331 en_US eng The Paleontological Society http://www.jstor.org/stable/1304740 Journal of Paleontology Knoll, Andrew H. 1984. Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard. Journal of Paleontology 58(1): 131-162. 0022-3360 http://nrs.harvard.edu/urn-3:HUL.InstRepos:4554331 http://www.journalofpaleontology.org/ 1984 ftharvardudash 2022-04-04T12:36:42Z A distinctive carbonate shallowing-upward sequence occurs within the Upper Riphean (750-800 Ma) Hunnberg Formation of Nordaustlandet, Svalbard. Clastic limestones deposited in an open coastal marine environment pass upward into columnar stromatolitic bioherms, and these, in turn, are overlain by finely laminated lagoonal dolomites. Early diagenetic silicification has preserved microbiotas in each of the three major facies. The lagoonal biota includes a low diversity planktonic assemblage in which two species are overwhelmingly dominant. In strong contrast, the plankton assemblage found in open coastal cherts contains more than two dozen taxa. Importance values are far more equably distributed in this assemblage. Few microfossils are preserved in the biohermal stromatolites, but intercolumnar spaces contain abundant fossils whose taxonomic composition and abundance distribution is intermediate between those of the open coastal and lagoonal biotas. Fossil assemblages of the Hunnberg Formation are useful biostratigraphically; the open coastal plankton biota is clearly latest Riphean in aspect. They also contribute to our understanding of the paleoecological distribution of late Precambrian plankton. This distribution is of potential value in paleoenvironmental reconstruction and is equally important in helping to define the ecological context in which evolutionary interpretations of early microbes must be made. The Hunnberg biota is also important in that it combines features of both "chert facies" and "shale facies" Proterozoic microbiotas and, thus, helps to elucidate the similarities and differences between these two types of microfossil assemblages. The Hunnberg microbiota contains 33 taxa, of which two are formally described as new: Cymatiosphaeroides kullingii n. gen. et n. sp. and Trachyhystri-chosphaera vidalii n. sp. Organismic and Evolutionary Biology Other/Unknown Material Nordaustlandet Svalbard Harvard University: DASH - Digital Access to Scholarship at Harvard Nordaustlandet ENVELOPE(22.400,22.400,79.800,79.800) Svalbard
institution Open Polar
collection Harvard University: DASH - Digital Access to Scholarship at Harvard
op_collection_id ftharvardudash
language English
topic http://www.journalofpaleontology.org/
spellingShingle http://www.journalofpaleontology.org/
Knoll, Andrew
Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
topic_facet http://www.journalofpaleontology.org/
description A distinctive carbonate shallowing-upward sequence occurs within the Upper Riphean (750-800 Ma) Hunnberg Formation of Nordaustlandet, Svalbard. Clastic limestones deposited in an open coastal marine environment pass upward into columnar stromatolitic bioherms, and these, in turn, are overlain by finely laminated lagoonal dolomites. Early diagenetic silicification has preserved microbiotas in each of the three major facies. The lagoonal biota includes a low diversity planktonic assemblage in which two species are overwhelmingly dominant. In strong contrast, the plankton assemblage found in open coastal cherts contains more than two dozen taxa. Importance values are far more equably distributed in this assemblage. Few microfossils are preserved in the biohermal stromatolites, but intercolumnar spaces contain abundant fossils whose taxonomic composition and abundance distribution is intermediate between those of the open coastal and lagoonal biotas. Fossil assemblages of the Hunnberg Formation are useful biostratigraphically; the open coastal plankton biota is clearly latest Riphean in aspect. They also contribute to our understanding of the paleoecological distribution of late Precambrian plankton. This distribution is of potential value in paleoenvironmental reconstruction and is equally important in helping to define the ecological context in which evolutionary interpretations of early microbes must be made. The Hunnberg biota is also important in that it combines features of both "chert facies" and "shale facies" Proterozoic microbiotas and, thus, helps to elucidate the similarities and differences between these two types of microfossil assemblages. The Hunnberg microbiota contains 33 taxa, of which two are formally described as new: Cymatiosphaeroides kullingii n. gen. et n. sp. and Trachyhystri-chosphaera vidalii n. sp. Organismic and Evolutionary Biology
author Knoll, Andrew
author_facet Knoll, Andrew
author_sort Knoll, Andrew
title Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
title_short Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
title_full Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
title_fullStr Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
title_full_unstemmed Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard
title_sort microbiotas of the late precambrian hunnberg formation, nordaustlandet, svalbard
publisher The Paleontological Society
publishDate 1984
url http://nrs.harvard.edu/urn-3:HUL.InstRepos:4554331
long_lat ENVELOPE(22.400,22.400,79.800,79.800)
geographic Nordaustlandet
Svalbard
geographic_facet Nordaustlandet
Svalbard
genre Nordaustlandet
Svalbard
genre_facet Nordaustlandet
Svalbard
op_relation http://www.jstor.org/stable/1304740
Journal of Paleontology
Knoll, Andrew H. 1984. Microbiotas of the Late Precambrian Hunnberg Formation, Nordaustlandet, Svalbard. Journal of Paleontology 58(1): 131-162.
0022-3360
http://nrs.harvard.edu/urn-3:HUL.InstRepos:4554331
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