(Table 1) Abundance of radiolarians in the surface layer of bottom sediments from the Peru-Chile trench and shelf
Cobertura |
MEDIAN LATITUDE: -9.712100 * MEDIAN LONGITUDE: -79.280213 * SOUTH-BOUND LATITUDE: -10.550000 * WEST-BOUND LONGITUDE: -79.966700 * NORTH-BOUND LATITUDE: -9.193300 * EAST-BOUND LONGITUDE: -78.706700 * MINIMUM ELEVATION: -6250.0 m * MAXIMUM ELEVATION: -105.0 m |
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Data(s) |
20/12/1981
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Resumo |
Two radiolarian assemblages are distinguished: an equatorial sub-assemblage of the tropical assemblage in the East Pacific Ocean, which differs somewhat from association of radiolarians in the western part of the ocean, and an assemblage close to transitional one between the tropical and the boreal. The latter is characterized by presence of considerable number of species typical for cold-water regions. Some criteria are presented for distinguishing radiolarian associations in nearshore regions from similar associations in regions of the open ocean. |
Formato |
text/tab-separated-values, 8 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.755408 doi:10.1594/PANGAEA.755408 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: Kruglikova, Svetlana B (1981): Radiolarians in the surface layer of bottom sediments in the eastern part of the Pacific Ocean's tropical zone. Oceanology, 21(3), 359-363 |
Palavras-Chave | #Archive of Ocean Data; ARCOD; Bottle, Niskin; Counting, radiolarians; DM8; DM8-542; DM8-544; DM8-545; DM8-547; DM8-548; DM8-550; DM8-551; DM8-552; Dmitry Mendeleev; Elevation of event; Event label; Grab; GRAB; Latitude of event; Longitude of event; MULT; Multiple investigations; NIS; Radiolarians; Southeast Pacific |
Tipo |
Dataset |