Pleistocene deltaic sequence of Seline near Mala Paklenica - document of climatic oscillations.
Tihomir Marjanac, Ljerka Marjanac
Abstract
Tihomir Marjanac, Ljerka Marjanac
Abstract
Seline coastal section with well-exposed conglomerates and lacustrine sediments reveals complex depositional history during Pleistocene. Pleistocene succession studied is built of several deltaic bodies of Gilbert-type, divided by thin lacustrine sediments and paleosols. The whole succession is capped by thick lacustrine sediments. This contrasting depositional episodes record alternation of glacial pulses and melt-episodes, possibly of stadial-interstadial range.
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Seline coastal section with well-exposed conglomerates and lacustrine sediments reveals complex depositional history during Pleistocene. Pleistocene succession studied is built of several deltaic bodies of Gilbert-type, divided by thin lacustrine sediments and paleosols. The whole succession is capped by thick lacustrine sediments. This contrasting depositional episodes record alternation of glacial pulses and melt-episodes, possibly of stadial-interstadial range.
Key concepts: Stadial, Pleistocene, Sedimentary depositional environment, Geology, Paleontology, Ecological succession, Glacial period, Sequence (biology)