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Multiyear data on benthic foraminifera in a glaciated fjord of Svalbard. / Golikova, Elena; Kniazeva, Olga; Korsun, Sergei.

в: Data in Brief, Том 17, 04.2018, стр. 363-392.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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@article{ba57f4af798047bd87bfbae5a5995a69,
title = "Multiyear data on benthic foraminifera in a glaciated fjord of Svalbard",
abstract = "Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical glaciated fjord in West Spitsbergen (78°24′06″ N, 17°02′30″ E), has been sampled in summer 1995 and 2001–2007 for modern benthic foraminifera. We have normalized the abundances and unified the taxonomy of all these published and unpublished data sets and then compiled the record of foraminiferal assemblages changing over years into a comprehensive database. The record includes data on living and dead abundances of benthic foraminiferal species in the surface sediments (0–2 cm) and downcore abundances of living foraminifera (only for 2004). This database portrays benthic foraminifera, this key group of microfossils, in a gradually changing Arctic environment.",
keywords = "ENVIRONMENT, SPITSBERGEN",
author = "Elena Golikova and Olga Kniazeva and Sergei Korsun",
year = "2018",
month = apr,
doi = "10.1016/j.dib.2018.01.046",
language = "English",
volume = "17",
pages = "363--392",
journal = "Data in Brief",
issn = "2352-3409",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Multiyear data on benthic foraminifera in a glaciated fjord of Svalbard

AU - Golikova, Elena

AU - Kniazeva, Olga

AU - Korsun, Sergei

PY - 2018/4

Y1 - 2018/4

N2 - Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical glaciated fjord in West Spitsbergen (78°24′06″ N, 17°02′30″ E), has been sampled in summer 1995 and 2001–2007 for modern benthic foraminifera. We have normalized the abundances and unified the taxonomy of all these published and unpublished data sets and then compiled the record of foraminiferal assemblages changing over years into a comprehensive database. The record includes data on living and dead abundances of benthic foraminiferal species in the surface sediments (0–2 cm) and downcore abundances of living foraminifera (only for 2004). This database portrays benthic foraminifera, this key group of microfossils, in a gradually changing Arctic environment.

AB - Glaciers in the fjords of Svalbard have been receding over last decades. Tempelfjorden, a typical glaciated fjord in West Spitsbergen (78°24′06″ N, 17°02′30″ E), has been sampled in summer 1995 and 2001–2007 for modern benthic foraminifera. We have normalized the abundances and unified the taxonomy of all these published and unpublished data sets and then compiled the record of foraminiferal assemblages changing over years into a comprehensive database. The record includes data on living and dead abundances of benthic foraminiferal species in the surface sediments (0–2 cm) and downcore abundances of living foraminifera (only for 2004). This database portrays benthic foraminifera, this key group of microfossils, in a gradually changing Arctic environment.

KW - ENVIRONMENT

KW - SPITSBERGEN

UR - http://www.scopus.com/inward/record.url?scp=85041612038&partnerID=8YFLogxK

UR - http://www.mendeley.com/research/multiyear-data-benthic-foraminifera-glaciated-fjord-svalbard

U2 - 10.1016/j.dib.2018.01.046

DO - 10.1016/j.dib.2018.01.046

M3 - Article

C2 - 29876406

VL - 17

SP - 363

EP - 392

JO - Data in Brief

JF - Data in Brief

SN - 2352-3409

ER -

ID: 10447069