Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529

Sediment cores from the Fram Strait are dated by means of calcareous nannofossil biostratigraphy and are shown to represent, at the most, the last 300 kyr (oxygen isotope stages 1-8). Differences in sedimentation rates are mainly controlled by the bottom topography and the intensity of ice-rafted de...

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Bibliographic Details
Main Author: Gard, Gunilla
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1987
Subjects:
Gravity corer Kiel type
Piston corer BGR type
ARK-III/3
Polarstern
Silicon Cycling in the World Ocean SINOPS
Fram Strait
Online Access:https://dx.doi.org/10.1594/pangaea.735010
https://doi.pangaea.de/10.1594/PANGAEA.735010
id ftdatacite:10.1594/pangaea.735010
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735010 2023-05-15T16:18:00+02:00 Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529 Gard, Gunilla 1987 application/zip https://dx.doi.org/10.1594/pangaea.735010 https://doi.pangaea.de/10.1594/PANGAEA.735010 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1029/pa002i005p00519 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Gravity corer Kiel type Piston corer BGR type ARK-III/3 Polarstern Silicon Cycling in the World Ocean SINOPS Supplementary Collection of Datasets Collection article 1987 ftdatacite https://doi.org/10.1594/pangaea.735010 https://doi.org/10.1029/pa002i005p00519 2022-02-08T16:24:46Z Sediment cores from the Fram Strait are dated by means of calcareous nannofossil biostratigraphy and are shown to represent, at the most, the last 300 kyr (oxygen isotope stages 1-8). Differences in sedimentation rates are mainly controlled by the bottom topography and the intensity of ice-rafted deposition. Sedimentation rates are normally in the order of a few centimeters per kiloyear in the central Fram Strait but increase to over 10 cm/kyr in cores located on the continental slope. The highest sediment accumulation rates occurred on the shelf (several tens of centimeters per kiloyear). Article in Journal/Newspaper Fram Strait DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
Piston corer BGR type
ARK-III/3
Polarstern
Silicon Cycling in the World Ocean SINOPS
spellingShingle Gravity corer Kiel type
Piston corer BGR type
ARK-III/3
Polarstern
Silicon Cycling in the World Ocean SINOPS
Gard, Gunilla
Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
topic_facet Gravity corer Kiel type
Piston corer BGR type
ARK-III/3
Polarstern
Silicon Cycling in the World Ocean SINOPS
description Sediment cores from the Fram Strait are dated by means of calcareous nannofossil biostratigraphy and are shown to represent, at the most, the last 300 kyr (oxygen isotope stages 1-8). Differences in sedimentation rates are mainly controlled by the bottom topography and the intensity of ice-rafted deposition. Sedimentation rates are normally in the order of a few centimeters per kiloyear in the central Fram Strait but increase to over 10 cm/kyr in cores located on the continental slope. The highest sediment accumulation rates occurred on the shelf (several tens of centimeters per kiloyear).
format Article in Journal/Newspaper
author Gard, Gunilla
author_facet Gard, Gunilla
author_sort Gard, Gunilla
title Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
title_short Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
title_full Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
title_fullStr Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
title_full_unstemmed Abundance of calcareous nannofossils in sediments of the Fram Strait, supplement to: Gard, Gunilla (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529
title_sort abundance of calcareous nannofossils in sediments of the fram strait, supplement to: gard, gunilla (1987): late quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: fram strait, arctica. paleoceanography, 2(5), 519-529
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 1987
url https://dx.doi.org/10.1594/pangaea.735010
https://doi.pangaea.de/10.1594/PANGAEA.735010
genre Fram Strait
genre_facet Fram Strait
op_relation https://dx.doi.org/10.1029/pa002i005p00519
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/pangaea.735010
https://doi.org/10.1029/pa002i005p00519
_version_ 1766004030649139200

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