Biomass of seston in the benthic layer of the Southwestern Indian Ocean

Fuente: PANGAEA
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Autores principales: Rudyakov, Yury A, Vereshchaka, Alexander L, Vinogradov, Georgy M, Geptner, Mikhail V
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1990
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author Rudyakov, Yury A
Vereshchaka, Alexander L
Vinogradov, Georgy M
Geptner, Mikhail V
author_facet Rudyakov, Yury A
Vereshchaka, Alexander L
Vinogradov, Georgy M
Geptner, Mikhail V
collection Datos científicos de ciencias marinas y ambientales
contents At stations to 1530 m depth in the Mozambique Channel and on the Saya-de-Malha and Walters banks seston biomass 2 m above the bottom was lower than at 30 m. Above the Walters shoal this difference was 13.2 mg/m**3 and was not equal to zero for P < 0.001. These results contradict previous ideas of biomass increase in benthic layers. The most likely cause of the observed impoverishment of plankton may be predominant consumption of living zooplankton component of seston by bottom and near-bottom predators. In the area of the Walters shoal this consumption is estimated as being about 300 mg/m**2 per day. Animals inhabiting this area live mainly on plankton brought in by horizontal advection, so that existence of faunal assemblages even on shallow-water submarine elevations is supported not mainly by local photosynthesis, but by primary production of surrounding waters.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_758809
institution PANGAEA
language en
publishDate 1990
publisher PANGAEA
record_format pangaea
spellingShingle Biomass of seston in the benthic layer of the Southwestern Indian Ocean
Rudyakov, Yury A
Vereshchaka, Alexander L
Vinogradov, Georgy M
Geptner, Mikhail V
Archive of Ocean Data; ARCOD; HAI; Indian Ocean; Towed zooplankton net; Vy17-2593; Vy17-2624; Vy17-2626; Vy17-2627; Vy17-2629; Vy17-2635; Vy17-2636; Vy17-2647; Vy17-2649; Vy17-2655; Vy17-2660; Vy17-2661; Vy17-2676; Vy17-2678; Vy17-2681; Vy17-2687; Vy17-2691; Vy17-2700; Vy17-2703; Vy17-2709; Vy17-2737; Vy17-2741; Vy17-2743; Vy17-2746; Vy17-2757; Vy17-2760; Vy17-2763
At stations to 1530 m depth in the Mozambique Channel and on the Saya-de-Malha and Walters banks seston biomass 2 m above the bottom was lower than at 30 m. Above the Walters shoal this difference was 13.2 mg/m**3 and was not equal to zero for P < 0.001. These results contradict previous ideas of biomass increase in benthic layers. The most likely cause of the observed impoverishment of plankton may be predominant consumption of living zooplankton component of seston by bottom and near-bottom predators. In the area of the Walters shoal this consumption is estimated as being about 300 mg/m**2 per day. Animals inhabiting this area live mainly on plankton brought in by horizontal advection, so that existence of faunal assemblages even on shallow-water submarine elevations is supported not mainly by local photosynthesis, but by primary production of surrounding waters.
title Biomass of seston in the benthic layer of the Southwestern Indian Ocean
topic Archive of Ocean Data; ARCOD; HAI; Indian Ocean; Towed zooplankton net; Vy17-2593; Vy17-2624; Vy17-2626; Vy17-2627; Vy17-2629; Vy17-2635; Vy17-2636; Vy17-2647; Vy17-2649; Vy17-2655; Vy17-2660; Vy17-2661; Vy17-2676; Vy17-2678; Vy17-2681; Vy17-2687; Vy17-2691; Vy17-2700; Vy17-2703; Vy17-2709; Vy17-2737; Vy17-2741; Vy17-2743; Vy17-2746; Vy17-2757; Vy17-2760; Vy17-2763
url https://doi.org/10.1594/PANGAEA.758809