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: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.804515
https://doi.pangaea.de/10.1594/PANGAEA.804515
id ftdatacite:10.1594/pangaea.804515
record_format openpolar
spelling ftdatacite:10.1594/pangaea.804515 2024-09-15T18:16:08+00:00 Meroplankton in the Kara Sea ... Fetzer, Ingo 2012 application/zip https://dx.doi.org/10.1594/pangaea.804515 https://doi.pangaea.de/10.1594/PANGAEA.804515 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Siberian River Run-Off SIRRO article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.804515 2024-08-01T10:51:31Z 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. ... : 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 ... Article in Journal/Newspaper Kara Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Siberian River Run-Off SIRRO
spellingShingle Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Siberian River Run-Off SIRRO
Fetzer, Ingo
Meroplankton in the Kara Sea ...
topic_facet Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
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. ... : 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 ...
format Article in Journal/Newspaper
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://dx.doi.org/10.1594/pangaea.804515
https://doi.pangaea.de/10.1594/PANGAEA.804515
genre Kara Sea
genre_facet Kara Sea
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.804515
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