Age determination of ODP Hole 182-1127B (Table 1)

• Main Authors: Andres, Miriam S, Bernasconi, Stefano M, McKenzie, Judith A, Röhl, Ursula
• Format: Dataset
• Language: English
• Published: PANGAEA 2003
• Subjects: 182-1127B; Age; 14C AMS; 14C calibrated; dated; dated standard deviation; maximum/old; minimum/young; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Great Australian Bight; Joides Resolution; Leg182; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; Antarc*; Antarctic; ice core; Planktonic foraminifera; Southern Ocean
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.708217; https://doi.org/10.1594/PANGAEA.708217

In Northern Hemisphere deglaciation records, the transition from the last glacial to the Holocene indicates a rapid return to near-glacial conditions during the Younger Dryas, whereas their Southern Hemisphere ice core counterparts record two separate cooling events: the Antarctic Cold Reversal and the Oceanic Cold Reversal. Spatial distribution and relative timing of these events in both hemispheres are central for our understanding of causes and mechanisms of abrupt climate change. To date, no marine record from the southern mid-latitudes conclusively demonstrates that the Younger Dryas was a significant event in the Southern Ocean. Here, we present high-resolution oxygen isotope and iron content records of a radiocarbon-dated sedimentary sequence from the Great Australian Bight, which constrains oceanic and atmospheric changes during the last deglaciation. Oxygen isotopes from planktonic foraminifera indicate two rapid cold reversals (between 13.1 and 11.1 kyr BP) separated by a brief warming. The sedimentary iron content, interpreted as a proxy for wind strength, indicates a simultaneous change in atmospheric circulation pattern. Both records demonstrate the existence of cooling events in the Southern Hemisphere, which are synchronous with the Northern Hemisphere Younger Dryas cold reversal (between 12.9 and 11.5 kyr BP). Such evidence for the spatial distribution and timing of abrupt climatic fluctuations is essential data for groundtruthing results derived from global climate models.