Mid-late pleistocene benthic foraminifera from Southwestern South Atlantic: Driven by primary productivity or water mass properties?

In the Atlantic sector of the Southern Ocean up to 35°S, Neogene benthic foraminiferal faunal changes have been interpreted, alternatively, as changes in deep water-masses distribution and organic matter availability, in surface, the Southwestern South Atlantic presents a highly dynamic frontal zone...

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Autor principal: Chapori, N.G
Otros Autores: Laprida, C., Watanabe, S., Totah, V., Violante, R.A
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Publicado: Micropaleontology Press 2014
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100 1 |a Chapori, N.G. 
245 1 0 |a Mid-late pleistocene benthic foraminifera from Southwestern South Atlantic: Driven by primary productivity or water mass properties? 
260 |b Micropaleontology Press  |c 2014 
270 1 0 |m Chapori, N.G.; Instituto de Estudios Andinos Don Pablo Groeber, Departamento de Ciencias Geológicas, Ciudad Universitaria, Intendente Güiraldes 2160, Argentina 
506 |2 openaire  |e Política editorial 
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520 3 |a In the Atlantic sector of the Southern Ocean up to 35°S, Neogene benthic foraminiferal faunal changes have been interpreted, alternatively, as changes in deep water-masses distribution and organic matter availability, in surface, the Southwestern South Atlantic presents a highly dynamic frontal zone and exhibits large spatial and temporal variability in primary productivity that influences the export of organic carbon from the euphotic zone. However, below ∼1000 meters depth, it is characterized by the interaction of several water masses. For this reason, the western sector of the South Atlantic is a natural laboratory to test the benthic foraminifera's response to changes in both, the deep water-masses distribution and the exported productivity, in order to define which was the main factor controlling the benthic foraminiferal assemblages structure during a glacial Mid-Late Pleistocene event, abundance analysis of organic matter content, oxygen availability and water masses marker species, and Q-mode factor analysis were carried out on core SP1251 (3400m; ∼3S°S - 54°W). Our results indicate that the benthic foraminiferal assemblages are mainly composed of high organic matter and oxygen availability-associated species revealing that productivity has been the main factor in determining the stracture of the assemblages' composition. These results also reflect that surface productivity regime would have not been uniform as a result of variations in the shelfbreak up welling of Patagonia as a consequence of variations in the Antarctic upwelling.  |l eng 
536 |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, CONICET, PIP 2142001100100014 
593 |a Instituto de Estudios Andinos Don Pablo Groeber, Departamento de Ciencias Geológicas, Ciudad Universitaria, Intendente Güiraldes 2160, Buenos Aires, C1428EGA, Argentina 
593 |a Museo Argentino de Ciencias Naturales Bernardino Rivadavia, Av. Ángel Gallardo 47, Buenos Aires, C1405DJR, Argentina 
593 |a División de Geología Marina, Departamento de Oceanografía, Servicio de Hidrografía Naval, Av. Montes de Oca 212, Buenos Aires, C1270ABV, Argentina 
690 1 0 |a BENTHIC FORAMINIFERA 
690 1 0 |a MID-LATE PLEISTOCENE 
690 1 0 |a PALEOCEANOGRAPHY 
690 1 0 |a PRIMARY PRODUCTIVITY 
690 1 0 |a SOUTH ATLANTIC OCEAN 
690 1 0 |a ABUNDANCE 
690 1 0 |a BENTHIC FORAMINIFERA 
690 1 0 |a FAUNA 
690 1 0 |a NEOGENE 
690 1 0 |a ORGANIC CARBON 
690 1 0 |a PALEOCEANOGRAPHY 
690 1 0 |a PLEISTOCENE 
690 1 0 |a PRIMARY PRODUCTION 
690 1 0 |a UPWELLING 
690 1 0 |a WATER MASS 
690 1 0 |a ATLANTIC OCEAN 
690 1 0 |a ATLANTIC OCEAN (SOUTH) 
690 1 0 |a PATAGONIA 
690 1 0 |a FORAMINIFERA 
700 1 |a Laprida, C. 
700 1 |a Watanabe, S. 
700 1 |a Totah, V. 
700 1 |a Violante, R.A. 
773 0 |d Micropaleontology Press, 2014  |g v. 60  |h pp. 195-210  |k n. 2  |p Micropaleontology  |x 00262803  |t Micropaleontology 
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856 4 0 |u https://hdl.handle.net/20.500.12110/paper_00262803_v60_n2_p195_Chapori  |y Handle 
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999 |c 84958