The Blake Event recorded near the Eemian type locality – A diachronic onset of the Eemian in Europe

Autor: Sier, M.J., Peeters, J., Dekkers, M., Pares, J.M., Chang, L., Busschers, F.S., Cohen, K.M., Wallinga, J., Bunnik, F.P.M., Roebroeks, W., Coastal dynamics, Fluvial systems and Global change, Paleomagnetism, Geomorfologie, NWO-ALW Open: Climate impact on human evolution: age calibration of hominin sites and paleolakes drilling project
Přispěvatelé: Coastal dynamics, Fluvial systems and Global change, Paleomagnetism, Geomorfologie, NWO-ALW Open: Climate impact on human evolution: age calibration of hominin sites and paleolakes drilling project
Rok vydání: 2015
Předmět:
Zdroj: QUATERNARY GEOCHRONOLOGY
Quaternary Geochronology, 28, 12. Elsevier
QUATERNARY GEOCHRONOLOGY, 28, 12-28
Quaternary Geochronology, 28, 12-28
Quaternary Geochronology 28 (2015)
ISSN: 1871-1014
DOI: 10.1016/j.quageo.2015.03.003
Popis: Multidisciplinary analysis including paleomagnetic, sedimentologic, sea-level change, luminescence dating and palynologic research was performed on a 25m long orientated core taken at Rutten, close to Eemian key localities in the Netherlands. The main goal of our research was to test a possible delayed onset of temperate conditions in this region compared to Southern Europe, occurring within the Last Interglacial. The sediments revealed the presence of the paleomagnetic Blake Event in ca. 10m of lower-deltaic floodbasin sediments that contain a pollen record covering the Eemian. The position of the Blake Event in relation to the pollen stratigraphy concurs with the earlier studied Neumark Nord 2 site. Paleomagnetic correlation to core MD95-2042 off SW Iberia indicates ca. 5kyr diachroneity between the pollen-based onset of temperate interglacial conditions between northern and southern Europe. The onset of the Eemian in north-western and central Europe (ca. 121.0ka) post-dates the Marine Isotope Stage 6/5e transition by ca. 10kyr. In addition, the Rutten data provide evidence for a relatively long duration of the Blake Event of at least 8kyr. The late onset of the temperate conditions that define the base of the Eemian, imply that NW Europe with the Eemian type area is not the most suited region to define the beginning of the Last Interglacial and Late Pleistocene for global chronostratigraphic use. © 2015 Elsevier B.V.
Databáze: OpenAIRE