Meroplankton in the Kara Sea

Meroplankton was sampled at 11 stations in the southern Kara Sea and the Yenisei Estuary in September 2000. Larvae of 29 benthic taxa representing 10 higher groups were identified. Meroplankton was present at almost all stations and most depth levels. The two most abundant groups were Echinodermata...

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Main Author: Fetzer, Ingo
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.804515
https://doi.org/10.1594/PANGAEA.804515
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.804515
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.804515 2023-05-15T16:59:52+02:00 Meroplankton in the Kara Sea Fetzer, Ingo MEDIAN LATITUDE: 75.357757 * MEDIAN LONGITUDE: 80.874845 * SOUTH-BOUND LATITUDE: 72.566500 * WEST-BOUND LONGITUDE: 74.003283 * NORTH-BOUND LATITUDE: 76.936200 * EAST-BOUND LONGITUDE: 85.763217 * DATE/TIME START: 2000-09-04T05:53:00 * DATE/TIME END: 2000-09-18T09:43:00 2012-12-19 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.804515 https://doi.org/10.1594/PANGAEA.804515 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.804515 https://doi.org/10.1594/PANGAEA.804515 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Fetzer, Ingo (2003): Distribution of meroplankton in the southern Kara Sea in relation to local hydrographic pattern. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 195-212 AWI_Paleo Paleoenvironmental Reconstructions from Marine Sediments @ AWI Siberian River Run-Off SIRRO Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.804515 2023-01-20T07:32:50Z Meroplankton was sampled at 11 stations in the southern Kara Sea and the Yenisei Estuary in September 2000. Larvae of 29 benthic taxa representing 10 higher groups were identified. Meroplankton was present at almost all stations and most depth levels. The two most abundant groups were Echinodermata (68%) and Polychaeta (26%). Echinoderms dominated total meroplankton locally due to mass occurrences of Ophiopluteus larvae. The relative group composition was highly variable and seemed to depend mainly on the local hydrographic pattern. Comparison of meroplanktonic data with the distribution of the adults revealed for Spionida and Bivalvia a 'downstream' transport of the larvae whereas for other polychaete species and Ophiuroida 'upstream' transport into the estuary occurred. The distribution and concentration of the larvae within the estuary is explained by physical barriers established by hydrographic gradients, the prevailing mixing processes and the presence of a near-bottom counter current. Dataset Kara Sea PANGAEA - Data Publisher for Earth & Environmental Science Kara Sea ENVELOPE(74.003283,85.763217,76.936200,72.566500)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic AWI_Paleo
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Siberian River Run-Off
SIRRO
spellingShingle AWI_Paleo
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Siberian River Run-Off
SIRRO
Fetzer, Ingo
Meroplankton in the Kara Sea
topic_facet AWI_Paleo
Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Siberian River Run-Off
SIRRO
description Meroplankton was sampled at 11 stations in the southern Kara Sea and the Yenisei Estuary in September 2000. Larvae of 29 benthic taxa representing 10 higher groups were identified. Meroplankton was present at almost all stations and most depth levels. The two most abundant groups were Echinodermata (68%) and Polychaeta (26%). Echinoderms dominated total meroplankton locally due to mass occurrences of Ophiopluteus larvae. The relative group composition was highly variable and seemed to depend mainly on the local hydrographic pattern. Comparison of meroplanktonic data with the distribution of the adults revealed for Spionida and Bivalvia a 'downstream' transport of the larvae whereas for other polychaete species and Ophiuroida 'upstream' transport into the estuary occurred. The distribution and concentration of the larvae within the estuary is explained by physical barriers established by hydrographic gradients, the prevailing mixing processes and the presence of a near-bottom counter current.
format Dataset
author Fetzer, Ingo
author_facet Fetzer, Ingo
author_sort Fetzer, Ingo
title Meroplankton in the Kara Sea
title_short Meroplankton in the Kara Sea
title_full Meroplankton in the Kara Sea
title_fullStr Meroplankton in the Kara Sea
title_full_unstemmed Meroplankton in the Kara Sea
title_sort meroplankton in the kara sea
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.804515
https://doi.org/10.1594/PANGAEA.804515
op_coverage MEDIAN LATITUDE: 75.357757 * MEDIAN LONGITUDE: 80.874845 * SOUTH-BOUND LATITUDE: 72.566500 * WEST-BOUND LONGITUDE: 74.003283 * NORTH-BOUND LATITUDE: 76.936200 * EAST-BOUND LONGITUDE: 85.763217 * DATE/TIME START: 2000-09-04T05:53:00 * DATE/TIME END: 2000-09-18T09:43:00
long_lat ENVELOPE(74.003283,85.763217,76.936200,72.566500)
geographic Kara Sea
geographic_facet Kara Sea
genre Kara Sea
genre_facet Kara Sea
op_source Supplement to: Fetzer, Ingo (2003): Distribution of meroplankton in the southern Kara Sea in relation to local hydrographic pattern. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 195-212
op_relation https://doi.pangaea.de/10.1594/PANGAEA.804515
https://doi.org/10.1594/PANGAEA.804515
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.804515
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