Distribution of radiolarians and tintinnid ciliates in Upper Holocene sediments of Laptev and East Siberian seas
Interest in the study of microplanktonic organisms in the Arctic has increased owing to their direct participation in the process of sedimentation and sensitive response to changes in environmental and climatic factors. This study presents new data on the taxonomic diversity and content of radiolari...
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Veröffentlicht in: | Polar biology 2023, Vol.46 (1), p.35-51 |
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Zusammenfassung: | Interest in the study of microplanktonic organisms in the Arctic has increased owing to their direct participation in the process of sedimentation and sensitive response to changes in environmental and climatic factors. This study presents new data on the taxonomic diversity and content of radiolarian skeletons and agglutinated tintinnid ciliate loricae in the Upper Holocene sediments of the Laptev Sea, East Siberian Sea, and the adjacent part of the Arctic Ocean. We traced the spatial distribution of representative microfauna of these groups in surface sediments and sediment cores. Radiolarian skeletons were found in the surface sediments of the continental slope of the Laptev Sea and adjacent parts of the Arctic Ocean. These belong to the following six species:
Stylatractus
(?) sp.,
Actinomma leptoderma leptoderma, Actinomma leptoderma longispina
,
Streblacantha circumtexta
,
Spongotrochus glacialis
, and
Cycladophora davisiana
. The radiolarian fauna detected was in deep sea and close to the fauna of the Nansen Basin (Central Arctic). Furthermore, we found tintinnid ciliate loricae belonging to the following seven species:
Tintinnopsis ventricosoides
,
Tintinnopsis fimbriata
,
Tintinnopsis turbo
,
Tintinnopsis nitida
,
Tintinnopsis
sp. cf.
fusus
(?),
Tintinnopsis
sp., and
Stenosemella nivalis
. In the study area, the tintinnid ciliate loricae of these species were discovered for the first time and traced mainly in the coastal shelf zone, which can be explained by their ecology. The only exception is that of
T. nitida
, which was found only on the continental slope of the Laptev Sea. Our findings advance knowledge on the biodiversity of Arctic seas and can be used to monitor ecological and paleoceanographic changes in the Arctic region. |
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ISSN: | 0722-4060 1432-2056 |
DOI: | 10.1007/s00300-022-03108-2 |