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Registros recuperados: 4
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Extent and retreat history of the Barra Fan Ice Stream offshore western Scotland and northern Ireland during the last glaciation ArchiMer
Callard, S. Louise; Cofaigh, Colm O.; Benetti, Sara; Chiverrell, Richard C.; Van Landeghem, Katrien J. J.; Saher, Margot H.; Gales, Jenny A.; Small, David; Clark, Chris D.; Stephen, J. Livingstone; Fabel, Derek; Moreton, Steven G..
During the Last Glacial Maximum (LGM) the marine-terminating Barra Fan Ice Stream (BFIS), a major conduit of the British Irish Ice Sheet (BITS), drained much of western Scotland and northwest Ireland with ice streaming onto the continental shelf of the Malin Sea. The extent and retreat history of this ice stream across the shelf, until now, is not well known. In particular, geochronological constraints on the history of this ice stream have thus far been restricted to deep-sea cores or terrestrial cosmogenic nuclide dating onshore, with ages across the shelf absent. To understand the possible external forcing factors acting on this marine terminating ice stream during retreat, improved geochronological constraint on its deglaciation is necessary. Here, we...
Tipo: Text Palavras-chave: British-Irish Ice Sheet; Glacimarine; Last glacial maximum; Radiocarbon dating; Ice-sheet retreat; Grounding-zone wedges.
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00504/61588/65891.pdf
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Evolution of the danube deep-sea fan since the last glacial maximum: New insights into Black Sea water-level fluctuations ArchiMer
Constantinescu, Adriana; Toucanne, Samuel; Dennielou, Bernard; Jorry, Stephan; Mulder, T.; Lericolais, Gilles.
The Danube Deep-Sea Fan (NW Black Sea) is one of the most developed deep-sea sediment depositional systems in Europe. Although the morphology and the architecture have been widely described in the past years, little is known about the stratigraphy of this depositional system. For the late Quaternary, this results from the lack of significant stratigraphic markers, the scarcity of radiocarbon ages and the difficulty in constraining reservoir ages. Recent robust quantification of reservoir ages has allowed the construction of a new stratigraphic framework for the Black Sea from the end of the last glacial period to the Holocene, thus giving the opportunity to correlate sedimentological and geochemical features previously described on the NW Black Sea margin...
Tipo: Text Palavras-chave: Danube deep-sea fan; Turbidites; Stratigraphy; Last glacial maximum; Termination 1; Water-level fluctuations.
Ano: 2015 URL: https://archimer.ifremer.fr/doc/00271/38236/64238.pdf
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Beyond skepticism: uncovering cryptic refugia using multiple lines of evidence ArchiMer
De Lafontaine, Guillaume; Amasifuen Guerra, Carlos Alberto; Ducousso, Alexis; Sanchez-goni, Maria-fernanda; Petit, Remy J..
The increasingly popular opinion that temperate plant and animal species persisted in many small refugia in Europe north of the main southern peninsular refugia directly challenges a classical paradigm. As indirect evidence for the existence of such glacial microrefugia readily accumulates, it is interesting to note that the few direct in situ occurrences of fossils testifying their local existence are almost always debated. Our recent study on European beech (Fagus sylvatica) refugia in south-western France was no exception to this trend. Yet, as mentioned by the philosopher Bertrand Russell, it is not possible ‘to get anywhere if we start from skepticism. We must start from a broad acceptance of whatever seems to be knowledge and is not rejected for some...
Tipo: Text Palavras-chave: Cryptic glacial refugia; Fagus sylvatica (European beech); Genetic structure; Heinrich stadials 1 and 2; Last glacial maximum; Late Pleniglacial interval; Microrefugia; Soil macrofossil charcoal.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00289/40066/38821.pdf
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Extreme temporal interpolation of sparse data is not a sufficient basis to substantiate a claim to have uncovered Pleistocene forest microrefugia ArchiMer
Huntley, Brian.
Tipo: Text Palavras-chave: Fagus sylvatica (beech); Heinrich Events 1 and 2; Landes de Gascogne; Last glacial maximum; Last glacial stage; Late Pleniglacial; Soil charcoal.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00289/40065/39263.pdf
Registros recuperados: 4
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