Detection and Characterisation of Eemian Marine Tephra Layers within the Sapropel S5 Sediments of the Aegean and Levantine Seas
The Eemian was the last interglacial period (~130 to 115 ka BP) to precede the current interglacial. In Eastern Mediterranean marine sediments, it is marked by a well-developed and organic-rich “sapropel” layer (S5), which is thought to reflect an intensification and northward mi...
Main Authors: | Christopher Satow, Katharine M. Grant, Sabine Wulf, Hartmut Schulz, Addison Mallon, Ian Matthews, John Lowe |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2020-03-01
|
Series: | Quaternary |
Subjects: | |
Online Access: | https://www.mdpi.com/2571-550X/3/1/6 |
Similar Items
-
River response to climate and sea level changes during the Late Saalian/Early Eemian in northern Poland – a case study of meandering river deposits in the Chłapowo cliff section
by: Moskalewicz Damian, et al.
Published: (2016-03-01) -
Magnetic studies of tephra in late Holocene peats and loessic soils from SE Iceland
by: Xia, Dunsheng
Published: (2002) -
History of the development of Eemian Interglacial lakes on the basis of Cladocera subfossil analysis (Central and Eastern Poland)
by: Niska Monika
Published: (2015-09-01) -
Dating peat profiles using tephra: stratigraphy, geochemistry and chronology
by: G.T. Swindles, et al.
Published: (2010-11-01) -
The East Asian Summer Monsoon : A comparison of present, Holocene and Eemian climate
by: Jacobson, Holger
Published: (2014)