Reconstructions of deltaic environments from Holocene palynological records in the Volga delta, northern Caspian Sea
| Autor: | R.M. Hoogendoorn, Salomon B. Kroonenberg, Nataliya S. Bolikhovskaya, Keith Richards, Suzanne A.G. Leroy, John Athersuch |
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| Přispěvatelé: | Ecosystem and Landscape Dynamics (IBED, FNWI) |
| Jazyk: | angličtina |
| Rok vydání: | 2014 |
| Předmět: |
Delta
Palynology Archeology Global and Planetary Change Vegetation and climate Ecology biology Dinoflagellate cysts and ostracods Paleontology biology.organism_classification law.invention Pollen and spores law Ostracod Period (geology) Aeolian processes Caspian Sea Sea level change Radiocarbon dating Sea level Holocene Geology Volga delta Earth-Surface Processes |
| Zdroj: | Holocene, 24(10), 1226-1252. SAGE Publications Ltd |
| ISSN: | 0959-6836 |
| Popis: | This article was made available through open access by the Brunel Open Access Publishing Fund. New palynological and ostracod data are presented from the Holocene Volga delta, obtained from short cores and surface samples collected in the Damchik region, near Astrakhan, Russian Federation in the northern Caspian Sea. Four phases of delta deposition are recognized and constrained by accelerated mass spectrometry (AMS) radiocarbon ages. Palynological records show that erosive channels, dunes (Baer hills) and inter-dune lakes were present during the period 11,500–8900 cal. BP at the time of the Mangyshlak Caspian lowstand. The period 8900–3770 cal. BP was characterized regionally by extensive steppe vegetation, with forest present at times with warmer, more humid climates, and with halophytic and xerophytic vegetation present at times of drought. The period 3770–2080 cal. BP was a time of active delta deposition, with forest or woodland close to the delta, indicating relatively warm and humid climates and variable Caspian Sea levels. From 2080 cal. BP to the present-day, aquatic pollen is frequent in highstand intervals and herbaceous pollen and fungal hyphae frequent in lowstand intervals. Soils and incised valley sediments are associated with the regional Derbent regression and may be time-equivalent with the ‘Medieval Warm Period’. Fungal spores are an indicator of erosional or aeolian processes, whereas fungal hyphae are associated with soil formation. Freshwater algae, ostracods and dinocysts indicate mainly freshwater conditions during the Holocene with minor brackish influences. Dinocysts present include Spiniferites cruciformis, Caspidinium rugosum, Impagidinium caspienense and Pterocysta cruciformis, the latter a new record for the Caspian Sea. The Holocene Volga delta is a partial analogue for the much larger oil and gas bearing Mio-Pliocene palaeo-Volga delta. Funding for the data collection and field work was provided from the following sources: 1 – IGCP-UNESCO 2003–2008 (Project 481 CASPAGE, Dating Caspian Sea Level Change); 2 – NWO, Netherlands Science Foundation and RFFI, Russian Science Foundation 2005–2008 (Programme: ‘VHR Seismic Stratigraphy and Paleoecology of the Holocene Volga Delta’); and 3 – BP Exploration (Caspian Sea) Sea Ltd. (Azeri-Chirag-Gunashli) 2005–2008 (‘Unravelling the Small-Scale Stratigraphy and Sediment Dynamics of the Modern Volga Delta Using VHR Marine Geophysics’). The palynological work was funded jointly by BP Exploration (Caspian Sea) Ltd., Delft University of Technology and KrA Stratigraphic Ltd. Ostracod analyses were funded by StrataData Ltd. and funding for two additional radiocarbon dates provided by Deltares. |
| Databáze: | OpenAIRE |
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