Abstract

Lake Towuti is located on central Sulawesi/Indonesia, within the Indo Pacific Warm Pool, a globally important region for atmospheric heat and moisture budgets. In 2015 the Towuti Drilling Project recovered more than 1000 m of drill core from the lake, along with downhole geophysical logging data from two drilling sites. The cores constitute the longest continuous lacustrine sediment succession from the Indo Pacific Warm Pool. We combined lithological descriptions with borehole logging data and used multivariate statistics to better understand the cyclic sequence, paleoenvironments, and geochronology of these sediments. Accurate chronologies are crucial to analyze and interpret paleoclimate records. Astronomical tuning can help build age-depth models and fill gaps between age control points. Cyclostratigraphic investigations were conducted on a downhole magnetic susceptibility log from the lacustrine facies (10–98 m below lake floor) from a continuous record of sediments in Lake Towuti. This study provides insights into the sedimentary history of the basin between radiometric ages derived from dating a tephra layer (~ 797 ka) and C14-ages (~ 45 ka) in the cores. We derived an age model that spans from late marine isotope stage (MIS) 23 to late MIS 6 (903 ± 11 to 131 ± 67 ka). Although uncertainties caused by the relatively short record and the small differences in the physical properties of sediments limited the efficacy of our approach, we suggest that eccentricity cycles and/or global glacial-interglacial climate variability were the main drivers of local variations in hydroclimate in central Indonesia. We generated the first nearly complete age-depth model for the lacustrine facies of Lake Towuti and examined the potential of geophysical downhole logging for time estimation and lithological description. Future lake drilling projects will benefit from this approach, since logging data are available just after the drilling campaign, whereas core descriptions, though more resolved, only become available months to years later.

Highlights

  • Lake Towuti is part of the Malili Lake System in central Sulawesi, Indonesia

  • Uncertainties caused by the relatively short record and the small differences in the physical properties of sediments limited the efficacy of our approach, we suggest that eccentricity cycles and/or global glacial-interglacial climate variability were the main drivers of local variations in hydroclimate in central Indonesia

  • We focused on the magnetic susceptibility (MS) record of Site 1, where, in contrast to Site 2, occurrence of movement deposits (MMD) is minor

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Summary

Introduction

Lake Towuti is part of the Malili Lake System in central Sulawesi, Indonesia. It is located within the Indo Pacific Warm Pool (IPWP), one of the most relevant regions for global climate variability on Earth. MIS 3 and 1 represent wet climate conditions and are marked by low magnetic susceptibility, whereas the drier MIS 2 is characterized by high susceptibility values (Tamuntuan et al 2014) Assuming this relation continues with depth, together with the observation that initial data from the long ICDP core and borehole logging show clear indications of orbital-scale climate variability during the middle to late Pleistocene (Russell et al 2016), it is likely that magnetic susceptibility values from downhole measurements are a promising variable that can be used to investigate long-term climate change around Lake Towuti

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