Marinopalynological Evidence for the Late Quaternary Vegetation and Climatic Changes Along the Bulgarian Black Sea Coast

Atanassova, Juliana; Bozilova, Elissaveta

doi:10.1007/978-94-011-5274-7_4

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2005

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“…The aim of this paper is to summarize investigations of the palynology and contents of dinoflagellate cysts of ten cores from the deep, western part of the Black Sea (Atanassova, 1990(Atanassova, , 1995a(Atanassova, , 1995b(Atanassova, , 1999(Atanassova, , 2002Atanassova andBozilova, 1992, 1998;Shopov et al, 1992). The Black Sea deep-water sediment sequences provide long and continuous detailed records of changes in the biological and lithological environment in contrast to the shelf sequences, where a hiatus in the early Holocene sediments exists.…”

Section: Introductionmentioning

confidence: 99%

Palaeoecological setting of the western Black Sea area during the last 15000 years

Atanassova

2005

The Holocene

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Analysis of pollen, dinoflagellate cysts and lithology was carried out on ten cores from the western deep Black Sea and combined with radiocarbon dating to reconstruct the vegetation, climate and palaeoecological conditions. All the cores record a consistent sequence of Lateglacial and early Holocene steppe vegetation, which persisted until about 7100-7500 yr BP when Quercus, Corylus, Tilia and other temperate trees expanded, at about the same time as the influx of Mediterranean waters that resulted in sapropel deposition in the deep Black Sea. The sequence implies dry climatic conditions and a low level of the Black Sea during the early Holocene.

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Section: Introductionmentioning

confidence: 99%

Palaeoecological setting of the western Black Sea area during the last 15000 years

Atanassova

2005

The Holocene

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Marinopalynological Evidence for the Late Quaternary Vegetation and Climatic Changes Along the Bulgarian Black Sea Coast

Cited by 1 publication

References 1 publication

Palaeoecological setting of the western Black Sea area during the last 15000 years

Palaeoecological setting of the western Black Sea area during the last 15000 years

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