Holocene neoglacial events in the Bransfield Strait (Antarctica). Palaeocenographic and palaeoclimatic significance.

  1. Bárcena Pernía, María Ángeles
  2. Fabrés Francés, Joan
  3. Isla, E.
  4. Flores Villarejo, José Abel
  5. Sierro Sánchez, Francisco Javier
Revista:
Scientia Marina

ISSN: 0214-8358

Año de publicación: 2006

Volumen: 70

Número: 4

Páginas: 607-619

Tipo: Artículo

DOI: 10.3989/SCIMAR.2006.70N4607 DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Scientia Marina

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Resumen

Geochemical analysis, micropalaeontological analysis and radiometric dating techniques were performed on four gravity cores, G-1, G-2, A-3 and A-6, recovered during the BIO Hesperides expeditions GEBRA-93 and FRUELA-96 from the Bransfield Strait (Antarctica). Moreover, in order to improve the sedimentation rate control we tentatively relate abundance variations in the sea-ice taxa group (SITG) to air temperature estimations based on Deuterium contents in Vostok ice-core. The results of diatom analyses were related to the sequence of neoglacial events that have occurred over the last three millennia. For these periods, a restricted communication between the Weddell, Bransfield and Bellingshausen seas has been proposed. The abundance patterns of diatom valves, resting spores (RS) of the diatom Chaetoceros and opal content agree with the high productivity values previously reported for the area. The significant reduction Chaetoceros RS towards the present is interpreted as a reduction in surface productivity. Trend differences between Chaetoceros RS and TOC contents are explained in terms of organic matter preservation. Diatom communities from the Bransfield Strait did not play an important role in the global CO2 cycle during cold periods. Bio- and geochemical changes have overprinted high frequency cyclicity at about 200-300 yr, which might be related to the 200-yr solar cycle.