Temperature reconstruction for the Mid-Pleistocene Transition based on deep-dwelling foraminifera of IODP Site339-U1385, supplement to: Bahr, André; Kaboth, Stefanie; Hodell, David A; Zeeden, Christian; Fiebig, Jens; Friedrich, Oliver (2018): Oceanic heat pulses fueling moisture transport towards continental Europe across the mid-Pleistocene transition. Quaternary Science Reviews, 179, 48-58

André Bahr, Stefanie Kaboth, David A Hodell, Christian Zeeden, Jens Fiebig & Oliver Friedrich
The mid-Pleistocene Transition (MPT; approx. 1.2-0.7 Ma), is characterized by growing Northern Hemisphere ice sheets and the shift from a 41 kyr to a 100 kyr glacial-interglacial cyclicity. Concomitant to the growth of large ice sheets, atmospheric and oceanic circulation pattern have changed. One key feature of the North Atlantic is the wind-driven Subtropical Gyre, a major provider of heat and moisture for continental Europe. Here, we investigate changes in the strength and spatial configuration...
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