Tropical Indo-Pacific hydroclimate response to North Atlantic forcing during the last deglaciation as recorded by a speleothem from Sumatra, Indonesia

• Published in: Earth and Planetary Science Letters
• Main Authors: Wurtzel, Jennifer, Abram, Nerilie, Lewis, Sophie, Bajo, Petra, Hellstrom, John Charles, Troitzsch, Ulrike, Heslop, David
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier
• Subjects: speleothem; oxygen isotopes; Indo-Pacific; Younger Dryas; ITCZ; deglaciation; Austral; Indian; Pacific; North Atlantic
• Online Access: http://hdl.handle.net/1885/257115; https://doi.org/10.1016/j.epsl.2018.04.001; https://openresearch-repository.anu.edu.au/bitstream/1885/257115/3/01_Wurtzel_Tropical_Indo-Pacific_2018.pdf.jpg

Abrupt changes in Atlantic Meridional Overturning Circulation are known to have affected the strength of the Indian and Asian Monsoons during glacial and deglacial climate states. However, there is still much uncertainty around the hydroclimate response of the Indo-Pacific Warm Pool (IPWP) region to abrupt climate changes in the North Atlantic. Many studies suggest a mean southward shift in the intertropical convergence zone (ITCZ) in the IPWP region during phases of reduced Atlantic meridional overturning, however, existing proxies have seasonal biases and conflicting responses, making it difficult to determine the true extent of North Atlantic forcing in this climatically important region. Here we present a precisely-dated, high-resolution record of eastern Indian Ocean hydroclimate variability spanning the last 16 ky (thousand years) from O measurements in an aragonite–calcite speleothem from central Sumatra. This represents the western-most speleothem record from the IPWP region. Precipitation arrives year-round at this site, with the majority sourced from the local tropical eastern Indian Ocean and two additional long-range seasonal sources associated with the boreal and austral summer monsoons. The Sumatran speleothem demonstrates a clear deglacial structure that includes 18O enrichment during the Younger Dryas and 18O depletion during the Bølling–Allerød, similar to the pattern seen in speleothems of the Asian and Indian monsoon realms. The speleothem O changes at this site are best explained by changes in rainfall amount and changes in the contributions from different moisture pathways. Reduced rainfall in Sumatra during the Younger Dryas is most likely driven by reductions in moisture transport along the northern or southern monsoon transport pathways to Sumatra. Considered with other regional proxies, the record from Sumatra suggests the response of the IPWP to North Atlantic freshwater forcing is not solely driven by southward shifts of the ITCZ, but also a reduction in moisture transport along both ...