Neogene planktonic foraminifera of DSDP Leg 41 holes ...

During Leg 41 Neogene sediments were recovered from five sites off northwest Africa.On the Sierra Leone Rise (Site 366), Neogene sediments consist of nanno oozes, nanno chalk, and calcareous clays 230 meters thick, resting conformably on the late Oligocene sediments. The common succession of zones o...

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Main Authors: Krasheninnikov, Valery A, Pflaumann, Uwe
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1978
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.758432
https://doi.pangaea.de/10.1594/PANGAEA.758432
id ftdatacite:10.1594/pangaea.758432
record_format openpolar
spelling ftdatacite:10.1594/pangaea.758432 2024-09-15T18:31:03+00:00 Neogene planktonic foraminifera of DSDP Leg 41 holes ... Krasheninnikov, Valery A Pflaumann, Uwe 1978 application/zip https://dx.doi.org/10.1594/pangaea.758432 https://doi.pangaea.de/10.1594/PANGAEA.758432 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.41.112.1978 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg41 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1978 ftdatacite https://doi.org/10.1594/pangaea.75843210.2973/dsdp.proc.41.112.1978 2024-08-01T10:58:30Z During Leg 41 Neogene sediments were recovered from five sites off northwest Africa.On the Sierra Leone Rise (Site 366), Neogene sediments consist of nanno oozes, nanno chalk, and calcareous clays 230 meters thick, resting conformably on the late Oligocene sediments. The common succession of zones occurs with two hiatuses. The lower gap corresponds to an interval around the lower/middle Miocene boundary (the Praeorbulina glomerosa and Orbulina suturalis-Globorotalia peri-pheroronda zones are absent) and the upper gap coincides with an interval around the middle/upper Miocene boundary (the Sphaeroidinellopsis sub-dehiscens-GIobigerina druryi, Globigerina nepenthes-Globorotalia siakensis and Globorotalia conlinuosa zones are missing).In the Cape Verde Basin (Site 367) deep-water Neogene turbidites (about 200-250 m thick) contain poor fauna of redeposited and sorted Cretaceous, Eocene, Oligocene, and Neogene species.On the Cape Verde Rise (Site 368) the Neogene section starts with slightly calcareous and ... : Supplement to: Krasheninnikov, Valery A; Pflaumann, Uwe (1978): Zonal stratigraphy of Neogene deposits of the eastern part of the Atlantic Ocean by means of planktonic foraminifers, Leg 41 Deep Sea Drilling Project. In: Lancelot, Y; Seibold, E; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Print Office), 41, 613-657 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg41
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg41
Glomar Challenger
Deep Sea Drilling Project DSDP
Krasheninnikov, Valery A
Pflaumann, Uwe
Neogene planktonic foraminifera of DSDP Leg 41 holes ...
topic_facet Drilling/drill rig
Leg41
Glomar Challenger
Deep Sea Drilling Project DSDP
description During Leg 41 Neogene sediments were recovered from five sites off northwest Africa.On the Sierra Leone Rise (Site 366), Neogene sediments consist of nanno oozes, nanno chalk, and calcareous clays 230 meters thick, resting conformably on the late Oligocene sediments. The common succession of zones occurs with two hiatuses. The lower gap corresponds to an interval around the lower/middle Miocene boundary (the Praeorbulina glomerosa and Orbulina suturalis-Globorotalia peri-pheroronda zones are absent) and the upper gap coincides with an interval around the middle/upper Miocene boundary (the Sphaeroidinellopsis sub-dehiscens-GIobigerina druryi, Globigerina nepenthes-Globorotalia siakensis and Globorotalia conlinuosa zones are missing).In the Cape Verde Basin (Site 367) deep-water Neogene turbidites (about 200-250 m thick) contain poor fauna of redeposited and sorted Cretaceous, Eocene, Oligocene, and Neogene species.On the Cape Verde Rise (Site 368) the Neogene section starts with slightly calcareous and ... : Supplement to: Krasheninnikov, Valery A; Pflaumann, Uwe (1978): Zonal stratigraphy of Neogene deposits of the eastern part of the Atlantic Ocean by means of planktonic foraminifers, Leg 41 Deep Sea Drilling Project. In: Lancelot, Y; Seibold, E; Gardner, JV; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Print Office), 41, 613-657 ...
format Article in Journal/Newspaper
author Krasheninnikov, Valery A
Pflaumann, Uwe
author_facet Krasheninnikov, Valery A
Pflaumann, Uwe
author_sort Krasheninnikov, Valery A
title Neogene planktonic foraminifera of DSDP Leg 41 holes ...
title_short Neogene planktonic foraminifera of DSDP Leg 41 holes ...
title_full Neogene planktonic foraminifera of DSDP Leg 41 holes ...
title_fullStr Neogene planktonic foraminifera of DSDP Leg 41 holes ...
title_full_unstemmed Neogene planktonic foraminifera of DSDP Leg 41 holes ...
title_sort neogene planktonic foraminifera of dsdp leg 41 holes ...
publisher PANGAEA
publishDate 1978
url https://dx.doi.org/10.1594/pangaea.758432
https://doi.pangaea.de/10.1594/PANGAEA.758432
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/dsdp.proc.41.112.1978
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.75843210.2973/dsdp.proc.41.112.1978
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