María Ángeles Bárcena

ORCID: 0000-0001-8261-2286
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Isotope Analysis in Ecology
  • Methane Hydrates and Related Phenomena
  • Marine and coastal ecosystems
  • Geological formations and processes
  • Paleontology and Stratigraphy of Fossils
  • Diatoms and Algae Research
  • Marine Biology and Ecology Research
  • Marine and environmental studies
  • Geological Studies and Exploration
  • Hydrocarbon exploration and reservoir analysis
  • Geological and Tectonic Studies in Latin America
  • Archaeology and ancient environmental studies
  • Arctic and Antarctic ice dynamics
  • Cryospheric studies and observations
  • Geological and Geophysical Studies Worldwide
  • Polar Research and Ecology
  • Pleistocene-Era Hominins and Archaeology
  • Oceanographic and Atmospheric Processes
  • Microbial Community Ecology and Physiology
  • Astro and Planetary Science
  • Archaeological and Historical Studies
  • Mediterranean and Iberian flora and fauna
  • Maritime and Coastal Archaeology
  • Archaeological and Geological Studies

Universidad de Salamanca
2013-2024

Universidad de Granada
2007

Down‐core samples of planktonic and benthic foraminifera were analyzed for oxygen carbon isotopes in International Marine Past Global Changes Study (IMAGES) core MD99‐2343 order to study the interactions between climate change Northern Hemisphere western Mediterranean thermohaline circulation at times Heinrich events (HE). Our results confirm antiphase correlation enhanced North Atlantic Deep Water formation low ventilation Mediterranean. However, this reveals that relationship deepwater was...

10.1029/2004pa001051 article EN Paleoceanography 2005-06-01

The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in northwestern Barents Sea has been investigated within two coordinated Spanish Italian projects framework International Polar Year (IPY) Activity 367, NICE STREAMS. investigation conducted using a multidisciplinary approach to study sediment cores positioned on high-resolution multibeam bathymetry TOPAS/CHIRP sub-bottom profiles. Core correlation age model were based 27 AMS 14C samples, rock magnetic...

10.1016/j.gloplacha.2013.10.008 article EN cc-by-nc-nd Global and Planetary Change 2013-10-29

We examined the total diatom flux and species composition, coccolith mass collected with a sediment trap between October 1993 January 2006 in northeastern entrance of Gulf Lions (North Western Mediterranean). The average daily fluxes (3 × 107 valves m2 d–1 6.1 108 coccoliths day−1, respectively) are comparable magnitude previously reported data sets other high productivity areas Mediterranean. temporal particle pattern reflected variations surface oceanographic conditions primary...

10.1093/plankt/fbt055 article EN Journal of Plankton Research 2013-06-14

Two gravity cores, Gebra-1 and Gebra-2 from the central eastern basins of Bransfield Strait, West Antarctica, consist mainly hemipelagic, laminated muds with black layers rich in sand-sized volcanic ash. Micropalaeontological (diatoms radiolarians) geochemical (organic inorganic) analyses, together radiometric dating (U/Th, 14 C 210 Pb) have been performed on both cores. AMS analyses Total Organic Carbon yielded a C-age older than expected, 2810 yr BP for core top 2596 Gebra-2. The downcore...

10.1017/s0954102098000364 article EN Antarctic Science 1998-09-01

Abstract The hydrography of the Indian‐Atlantic Ocean gateway has been connected to high‐latitude climate dynamics by oceanic and atmospheric teleconnections on orbital suborbital timescales. A wealth sedimentary records aiming at reconstructing late Pleistocene paleoceanography around southern African continent devoted understanding these linkages. Most are, however, clustered close South tip, with comparatively less attention areas under direct influence frontal zones Southern Ocean/South...

10.1002/2014pa002636 article EN other-oa Paleoceanography 2015-01-16

The Antarctic Peninsula is sensitive to climatic change due its northerly position and the relatively reduced volume character of ice cover. High-resolution palaeoclimatic records from Ant arctic cores extend back only 500 years. A record 2850 years in Bransfield Basin investigated through analysis sediment gravity floor central subbasin (core GEBRA-1) slope eastern GEBRA-2). Sedimentological, mineralogical geo chemical properties have been systematically measured, together with Accelerator...

10.1191/09596830094953 article EN The Holocene 2000-09-01
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