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Precipitation changes in the Mediterranean basin during the Holocene from terrestrial and marine pollen records: a model-data comparison ArchiMer
Peyron, Odile; Combourieu-nebout, Nathalie; Brayshaw, David; Goring, Simon; Andrieu-ponel, Valerie; Desprat, Stephanie; Fletcher, Will; Gambin, Belinda; Ioakim, Chryssanthi; Joannin, Sebastien; Kotthoff, Ulrich; Kouli, Katerina; Montade, Vincent; Pross, Jörg; Sadori, Laura; Magny, Michel.
Climate evolution of the Mediterranean region during the Holocene exhibits strong spatial and temporal variability, which is notoriously difficult for models to reproduce. We propose here a new proxy-based climate synthesis synthesis and its comparison -at a regional (similar to 100 km) level - with a regional climate model to examine (i) opposing northern and southern precipitation regimes and (ii) an east-to-west precipitation dipole during the Holocene across the Mediterranean basin. Using precipitation estimates in-ferred from marine and terrestrial pollen archives, we focus on the early to mid-Holocene (8000 to 6000 cal yr BP) and the late Holocene (4000 to 2000 cal yr BP), to test these hypotheses on a Mediterranean-wide scale. Special attention was...
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Ano: 2017 URL: https://archimer.ifremer.fr/doc/00420/53173/55186.pdf
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Advancing Santorini’s tephrostratigraphy: new glass geochemical data and improved marine-terrestrial tephra correlations for the past ∼360 kyrs ArchiMer
Wulf, Sabine; Keller, Jörg; Satow, Christopher; Gertisser, Ralf; Kraml, Michael; Grant, Katharine M.; Appelt, Oona; Vakhrameeva, Polina; Koutsodendris, Andreas; Hardiman, Mark; Schulz, Hartmut; Pross, Jörg.
The island of Santorini in the Aegean Sea is one of the world’s most violent active volcanoes. Santorini has produced numerous highly explosive eruptions over at least the past ∼360 kyrs that are documented by the island’s unique proximal tephra record. However, the lack of precise eruption ages and comprehensive glass geochemical datasets for proximal tephras has long hindered the development of a detailed distal tephrostratigraphy for Santorini eruptions. In light of these requirements, this study develops a distal tephrostratigraphy for Santorini covering the past ∼360 kyrs, which represents a major step forward towards the establishment of a tephrostratigraphic framework for the Eastern Mediterranean region. We present new EPMA glass geochemical data...
Tipo: Text Palavras-chave: Santorini; EPMA glass chemistry; Proximal tephra deposits; Marine tephrostratigraphy; Land-sea correlations; Eastern Mediterranean region.
Ano: 2020 URL: https://archimer.ifremer.fr/doc/00588/70039/67968.pdf
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