Search results for "Dansgaard-Oeschger"

showing 3 items of 3 documents

Productivity modes in the Mediterranean Sea during Dansgaard–Oeschger (20,000–70,000 yr ago) oscillations

2013

The study of planktonic organisms during abrupt climatic variations of the last glacial period (Dansgaard-Oeschger oscillations, D-O) may reveal important insights on climatic, oceanographic and biological interactions. Here we present planktic foraminifera and coccolithophore data collected at the Ocean Drilling Program Site 963 (Sicily Channel), with a mean sampling resolution of respectively 43.5 and 98.9. yr, over the interval between 70,000 and 20,000. yr ago. The paleoenvironmental reconstruction suggests that three different scenarios can be seen across each D-O cycle: 1. oligotrophic surface water and a deep thermocline for the early Interstadials; 2. a Deep Chlorophyll Maximum and …

010506 paleontology010504 meteorology & atmospheric sciencesCoccolithophoreMediterraneanOceanography01 natural sciencesForaminifera/dk/atira/pure/sustainabledevelopmentgoals/life_below_waterWater columnMediterranean seaPaleoproductivity Dansgaard–Oeschger Mediterranean Planktonic Foraminifera CoccolithophoresCoccolithophores14. Life underwaterStadialGlacial periodSDG 14 - Life Below WaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesDeep chlorophyll maximumbiologyPaleontologybiology.organism_classificationOceanography13. Climate actionClimatologyPlanktonic ForaminiferaDansgaard-OeschgerThermoclineGeologyPaleoproductivityPalaeogeography, Palaeoclimatology, Palaeoecology
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High-frequency modification of the central Mediterranean seafloor environment over the last 74 ka

2022

Here we present a high-resolution record of benthic foraminiferal assemblages for the last 74 kyr from the Sicily Channel Ocean Drilling Program Leg 160 Site 963. Benthic foraminiferal results are compared with geochemical (benthic and planktic δ18O and δ13C) and calcareous plankton data, previously acquired on the same marine core sediments. Within the succession, three benthic foraminifera compositional zones were defined. Temporal changes in the assemblages are interpreted in the context of the modification of subtropical and temperate climate systems that affected the Mediterranean thermohaline circulation. A close connection between bottom conditions in the Sicily Channel and eastern M…

Benthic foraminiferaDansgaard-Oeschger oscillationPaleontologySettore GEO/01 - Paleontologia E PaleoecologiaOceanographyEcology Evolution Behavior and SystematicsCompositional data analysiODP Site 963Earth-Surface Processes
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Climate oscillations and changes in freshwater budget of the central-eastern Mediterranean between 20,000 and 70,000 years ago

2011

Mediterranean Dansgaard-Oeschger oscillations
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