Compilation of sedimentation rates and smear slide analysis of DSDP sites ...

A history of Mesozoie and Cenozoic palaeoenvironments of the North Atlantie Oeean has been developed based on a detailed analysis of the temporal and spatial distribution of major pelagie sediment facies, of hiatuses. of bulk sediment accumulation rates, and of concentrations and fluxes of the main...

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Main Authors: Thiede, Jörn, Ehrmann, Werner
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.832271
https://doi.pangaea.de/10.1594/PANGAEA.832271
id ftdatacite:10.1594/pangaea.832271
record_format openpolar
spelling ftdatacite:10.1594/pangaea.832271 2024-02-04T10:02:18+01:00 Compilation of sedimentation rates and smear slide analysis of DSDP sites ... Thiede, Jörn Ehrmann, Werner 2014 application/zip https://dx.doi.org/10.1594/pangaea.832271 https://doi.pangaea.de/10.1594/PANGAEA.832271 en eng PANGAEA https://www.schweizerbart.de/publications/detail/isbn/9783510570157/Contributions_15_to_Sedimentology https://www.schweizerbart.de/publications/detail/isbn/9783510570157/Contributions_15_to_Sedimentology https://dx.doi.org/10.2312/reports-gpi.1986.16 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Deep Sea Drilling Project DSDP Quaternary Environment of the Eurasian North QUEEN Collection article Supplementary Publication Series of Datasets 2014 ftdatacite https://doi.org/10.1594/pangaea.83227110.2312/reports-gpi.1986.16 2024-01-05T01:44:53Z A history of Mesozoie and Cenozoic palaeoenvironments of the North Atlantie Oeean has been developed based on a detailed analysis of the temporal and spatial distribution of major pelagie sediment facies, of hiatuses. of bulk sediment accumulation rates, and of concentrations and fluxes of the main deep-sea sediment components. The depositional history of the North Atlantic can be subdivided into three major phase: (a) Late Jurassie and Early Cretaceous phase: clastic terrigenous and biogenic pelagic sediment components accumulated rapidly under highly productive surface water masses over the entire occan basin; (b) Late Cretaceous to Early Miocene phase: relatively little terrigenous and pelagic biogenic sediment reached the North Atlantic Ocean floor, intensive hiatus formation occurred at variable rates, and wide stretches of the deep-ocean floor were covered by slowly accumulating terrigenous muds: (c) Middle Miocene to Recent phase: accumulation rates of biogenic and terrigenous deep-sea sediment ... : Supplement to: Thiede, Jörn; Ehrmann, Werner (1986): Late Mesozoic and Cenozoic sediment flux to the central North Atlantic Ocean. In: Summerhayes, C P & Shackleton, N J (eds), North Atlantic Palaeoceanography, Geological Society Special Publication, 21, 3-15 ... Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Shackleton
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Deep Sea Drilling Project DSDP
Quaternary Environment of the Eurasian North QUEEN
spellingShingle Deep Sea Drilling Project DSDP
Quaternary Environment of the Eurasian North QUEEN
Thiede, Jörn
Ehrmann, Werner
Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
topic_facet Deep Sea Drilling Project DSDP
Quaternary Environment of the Eurasian North QUEEN
description A history of Mesozoie and Cenozoic palaeoenvironments of the North Atlantie Oeean has been developed based on a detailed analysis of the temporal and spatial distribution of major pelagie sediment facies, of hiatuses. of bulk sediment accumulation rates, and of concentrations and fluxes of the main deep-sea sediment components. The depositional history of the North Atlantic can be subdivided into three major phase: (a) Late Jurassie and Early Cretaceous phase: clastic terrigenous and biogenic pelagic sediment components accumulated rapidly under highly productive surface water masses over the entire occan basin; (b) Late Cretaceous to Early Miocene phase: relatively little terrigenous and pelagic biogenic sediment reached the North Atlantic Ocean floor, intensive hiatus formation occurred at variable rates, and wide stretches of the deep-ocean floor were covered by slowly accumulating terrigenous muds: (c) Middle Miocene to Recent phase: accumulation rates of biogenic and terrigenous deep-sea sediment ... : Supplement to: Thiede, Jörn; Ehrmann, Werner (1986): Late Mesozoic and Cenozoic sediment flux to the central North Atlantic Ocean. In: Summerhayes, C P & Shackleton, N J (eds), North Atlantic Palaeoceanography, Geological Society Special Publication, 21, 3-15 ...
format Article in Journal/Newspaper
author Thiede, Jörn
Ehrmann, Werner
author_facet Thiede, Jörn
Ehrmann, Werner
author_sort Thiede, Jörn
title Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
title_short Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
title_full Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
title_fullStr Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
title_full_unstemmed Compilation of sedimentation rates and smear slide analysis of DSDP sites ...
title_sort compilation of sedimentation rates and smear slide analysis of dsdp sites ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.832271
https://doi.pangaea.de/10.1594/PANGAEA.832271
geographic Shackleton
geographic_facet Shackleton
genre North Atlantic
genre_facet North Atlantic
op_relation https://www.schweizerbart.de/publications/detail/isbn/9783510570157/Contributions_15_to_Sedimentology
https://www.schweizerbart.de/publications/detail/isbn/9783510570157/Contributions_15_to_Sedimentology
https://dx.doi.org/10.2312/reports-gpi.1986.16
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.83227110.2312/reports-gpi.1986.16
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