Elsterian glacial period dating

Preko cijele Bosne proteže se Dinarski pojas, koji predstavlja izdignuto i blago, prema sjeveru, svedenu visiju koja se prema jugu strmo spušta.U vrijeme kada su paleolitske zajednice nastanjivale područje sjeverne Bosne, vladali su slični klimatski odnosi kao i danas, u smislu temperature, padavina i podjele na godišnja doba.Sedimentacija mezozojskih naslaga na teritoriji sjeverne Bosne ima potpuno razviće u tri geološke periode: trijasu, juri i kredi.Mezozojske naslage imaju najveće teritorijalno razviće i grade unutrašnju, centralnu i vanjsku zonu Dinarida.The ages of sediments directly overlying the Elsterian till are approximately 400 ka and prove that the first extensive Fennoscandian ice sheet extension during the Quaternary correlates with MIS 12 and not with MIS 10.Furthermore, the 400 ka old fluvial units contain Lower Paleolithic stone artefacts that document the first human appearance in the region. Une biochronologie des gisements est proposée à partir des associations fauniques et des stades évolutifs des espèces : Terra Amata (MIS 11), Lazaret (MIS 6), Caverna delle Fate (MIS 5 et 4), Madonna dell' Arma (MIS 5), Arma delle Manie (MIS 4), Santa ...Glacialconditions returned at 12.5 ± 1.5 ka (LG3) and were characterized by low air temperatures and glaciershrinking.The Holocene glacial phases (HOL1-3) are recorded only in the MK cirque, likely due to itstopographic attributes.

Late-glacial and Holocene history of the northeast Mediterranean mountain glaciers - New insights from in situ-produced 36Cl-based cosmic ray exposure dating of paleo-glacier deposits on Mount Olympus, Greece In this study, we present a new glacial chronology based on 20 in situ-produced 36Cl-based cosmic ray exposure datings from moraine boulders and bedrock from the Throne of Zeus (TZ) and Megala Kazania (MK) cirques on Mount Olympus. more In this study, we present a new glacial chronology based on 20 in situ-produced 36Cl-based cosmic rayexposure datings from moraine boulders and bedrock from the Throne of Zeus (TZ) and Megala Kazania(MK) cirques on Mount Olympus.

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The Late Holoceneglacier expansions, include a moraine stabilization phase (HOL2) at 2.5 ± 0.3 ka, during wet conditionsand solar insolation minima, while (HOL3) corresponds to the early part of the Little Ice Age(0.64 ± 0.08ka).

Our glacial chronology is coherent with glacial chronologies from several cirques alongthe northeast Mediterranean mountains and in pace with numerous proxies from terrestrial and marinesystems from the north Aegean Sea. Sjeverna Bosna se geografski nalazi u okviru centralnoeuropskog panonskog bazena i to na njegovoj južnoj granici. Sjeverna Bosna se geografski nalazi u okviru centralnoeuropskog panonskog bazena i to na njegovoj južnoj granici.

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