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Radiolarian fluxes from the southern Bay of Bengal: sediment trap results

หน่วยงาน National Institute Of Oceanography (NIO), India

รายละเอียด

ชื่อเรื่อง : Radiolarian fluxes from the southern Bay of Bengal: sediment trap results
นักวิจัย : Gupta, S.M. , Mohan, R. , Guptha, M.V.S.
คำค้น : fossil radiolaria , foraminifera , monsoons , palaeoceanography , sediment traps , surface temperature , seasonal variations
หน่วยงาน : National Institute Of Oceanography (NIO), India
ผู้ร่วมงาน : -
ปีพิมพ์ : 2545
อ้างอิง : Deep-Sea Research (I: Oceanographic Research Papers), Vol. 49(9); 1669-1688p. , http://drs.nio.org/drs/handle/2264/1394
ที่มา : -
ความเชี่ยวชาญ : -
ความสัมพันธ์ : -
ขอบเขตของเนื้อหา : -
บทคัดย่อ/คำอธิบาย :

A study of radiolarian fluxes collected during 1991-93 from time-series sediment traps deployed at 1071 and 3010 m water depth in the southern Bay of Bengal (SBBT) yielded 40 species/groups of radiolarians. Among the order Polycystina, the species of sub-order Spumellaria were by far the most abundant (approx. 95%) followed by sub-order Nassellaria (5%). This is contrary to reports from the Atlantic and Pacific Oceans and is attributed to the prevailing hyposaline condition resulting from the monsoonal rainfall. Higher radiolarian fluxes occurred during March-May, when moderate salinity and a high sea surface temperature (SST) regime prevailed at the trap site. R-mode cluster analysis of the radiolarian flux data revealed three assemblages represented by the cooler (1) and warmer (2) surface dwelling fauna (0-50 m) dominated by spumellarians, and a deeper dwelling (3) sub-surface fauna (50-100 m) associated with deep dwelling (more than 100 m) nassellarian species. Spongaster tetras tetras, a surface water radiolarian species, exhibited its preference for high SST and moderate salinity conditions during the pre-monsoon season (March-May). Radiolarian fluxes responded to seasonal changes in SST and salinity variations due to the monsoonal precipitation, and the freshwater runoff from the Indian rivers causing a hyposaline condition in the Bay of Bengal. Results imply that the radiolarian assemblages in the down core data may reveal the monsoonal history in the geological past.

บรรณานุกรม :
Gupta, S.M. , Mohan, R. , Guptha, M.V.S. . (2545). Radiolarian fluxes from the southern Bay of Bengal: sediment trap results.
    : National Institute Of Oceanography (NIO), India.
Gupta, S.M. , Mohan, R. , Guptha, M.V.S. . 2545. "Radiolarian fluxes from the southern Bay of Bengal: sediment trap results".
    : National Institute Of Oceanography (NIO), India.
Gupta, S.M. , Mohan, R. , Guptha, M.V.S. . "Radiolarian fluxes from the southern Bay of Bengal: sediment trap results."
    : National Institute Of Oceanography (NIO), India, 2545. Print.
Gupta, S.M. , Mohan, R. , Guptha, M.V.S. . Radiolarian fluxes from the southern Bay of Bengal: sediment trap results. : National Institute Of Oceanography (NIO), India; 2545.