NOAA/WDS Paleoclimatology - Borneo High Resolution Holocene Speleothem Oxygen Isotope Data

STUDY NOTES: Subannual oxygen isotope record in six Holocene time windows from stalagmite BA03, Bukit Assam Cave, Borneo, Malaysia, plus decadal average d18O and d13C (as plotted in Figure 3; added 9/14/2017). Provided Keywords: Holocene, ENSO, speleothem, oxygen isotopes. Six Holocene time windows are as follows: 2500 yr window: 349.270-400.030mm, 2386.36-2597.86 Cal. year BP 3300 yr window: 474.630-492.600mm, 3234.12-3383.87 Cal. year BP 5200 yr window: 743.770-754.450mm, 5161.41-5225.49 Cal. year BP 5700 yr window: 827.186-838.316mm, 5628.52-5708.02 Cal. year BP 6700 yr window: 940.150-959.800mm, 6583.78-6740.98 Cal. year BP 8200 yr window: 1054.680-1073.698mm, 8136.82-8316.72 Cal. year BP
ABSTRACT SUPPLIED BY ORIGINATOR: The El Nino-Southern Oscillation (ENSO) is the primary driver of interannual climate variability in the tropics and subtropics. Despite substantial progress in understanding ocean-atmosphere feedbacks that drive ENSO today, relatively little is known about its behavior on centennial and longer timescales. Paleoclimate records from lakes, corals, molluscs and deep-sea sediments generally suggest that ENSO variability was weaker during the mid-Holocene (4-6 kyrBP) than the late Holocene (0-4 kyrBP). However, discrepancies amongst the records preclude a clear timeline of Holocene ENSO evolution and therefore the attribution of ENSO variability to specific climate forcing mechanisms. Here we present d18O results from a U-Th dated speleothem in Malaysian Borneo sampled at sub-annual resolution. The d18O of Borneo rainfall is a robust proxy of regional convective intensity and precipitation amount, both of which are directly influenced by ENSO activity. Our estimates of stalagmite d18O variance at ENSO periods (2-7 yr) show a significant reduction in interannual variability during the mid-Holocene (3240-3380 and 5160-5230 yrBP) relative to both the late Holocene (2390-2590 yrBP) and early Holocene (6590-6730 yrBP). The Borneo results are therefore inconsistent with lacustrine records of ENSO from the eastern equatorial Pacific that show little or no ENSO variance during the early Holocene. Instead, our results support coral, mollusc and foraminiferal records from the central and eastern equatorial Pacific that show a mid-Holocene minimum in ENSO variance. Reduced mid-Holocene interannual d18O variability in Borneo coincides with an overall minimum in mean d18O from 3.5 to 5.5 kyrBP. Persistent warm pool convection would tend to enhance the Walker circulation during the mid-Holocene, which likely contributed to reduced ENSO variance during this period. This finding implies that both convective intensity and interannual variability in Borneo are driven by coupled air-sea dynamics that are sensitive to precessional insolation forcing. Isolating the exact mechanisms that drive long-term ENSO evolution will require additional high-resolution paleoclimatic reconstructions and further investigation of Holocene tropical climate evolution using coupled climate models.