Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk

Data files present information on the quantitative distribution of the polycystine radiolarian species in the Quaternary marine sediments from the subarctic areas. Dataset on the open North Atlantic north of 43 °N contains percentages of 35 abundant (> 1%) species in 145 samples of five sediment...

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Autor principal: Matul, Alexander
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2018
Materias:
Earth and Planetary Science
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5988337/
https://www.ncbi.nlm.nih.gov/pubmed/29876415
http://dx.doi.org/10.1016/j.dib.2018.01.041
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author Matul, Alexander
author_facet Matul, Alexander
author_sort Matul, Alexander
collection PubMed
description Data files present information on the quantitative distribution of the polycystine radiolarian species in the Quaternary marine sediments from the subarctic areas. Dataset on the open North Atlantic north of 43 °N contains percentages of 35 abundant (> 1%) species in 145 samples of five sediment cores. Dataset on the Sea of Okhotsk contains percentages of 31 abundant (> 1%) species in 794 samples of seven sediment cores. Dataset on the bottom surface sediments of the North Atlantic contains percentages of 35 abundant (> 1%) species in 78 grab and core-top samples. For the microscopic radiolarian analysis, the sediment fraction of > 40/50 μm was used.
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spelling pubmed-59883372018-06-06 Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk Matul, Alexander Data Brief Earth and Planetary Science Data files present information on the quantitative distribution of the polycystine radiolarian species in the Quaternary marine sediments from the subarctic areas. Dataset on the open North Atlantic north of 43 °N contains percentages of 35 abundant (> 1%) species in 145 samples of five sediment cores. Dataset on the Sea of Okhotsk contains percentages of 31 abundant (> 1%) species in 794 samples of seven sediment cores. Dataset on the bottom surface sediments of the North Atlantic contains percentages of 35 abundant (> 1%) species in 78 grab and core-top samples. For the microscopic radiolarian analysis, the sediment fraction of > 40/50 μm was used. Elsevier 2018-02-02 /pmc/articles/PMC5988337/ /pubmed/29876415 http://dx.doi.org/10.1016/j.dib.2018.01.041 Text en © 2018 The Authors http://creativecommons.org/licenses/by/4.0/ This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
spellingShingle Earth and Planetary Science
Matul, Alexander
Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title_full Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title_fullStr Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title_full_unstemmed Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title_short Distribution of the polycystine radiolarian species in the Quaternary sediment cores of the subarctic North Atlantic and Sea of Okhotsk
title_sort distribution of the polycystine radiolarian species in the quaternary sediment cores of the subarctic north atlantic and sea of okhotsk
topic Earth and Planetary Science
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5988337/
https://www.ncbi.nlm.nih.gov/pubmed/29876415
http://dx.doi.org/10.1016/j.dib.2018.01.041
work_keys_str_mv AT matulalexander distributionofthepolycystineradiolarianspeciesinthequaternarysedimentcoresofthesubarcticnorthatlanticandseaofokhotsk

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