气候变化领域集成服务门户(CCPortal): The late quaternary tectonic; biogeochemical; and environmental evolution of ferruginous Lake Towuti; Indonesia

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DOI	10.1016/j.palaeo.2020.109905
	The late quaternary tectonic; biogeochemical; and environmental evolution of ferruginous Lake Towuti; Indonesia
	Russell J.M.; Vogel H.; Bijaksana S.; Melles M.; Deino A.; Hafidz A.; Haffner D.; Hasberg A.K.M.; Morlock M.; von Rintelen T.; Sheppard R.; Stelbrink B.; Stevenson J.
发表日期	2020
ISSN	0031-0182
卷号	556
英文摘要	There is a paucity of long and continuous continental records from South East Asia suitable to inform on past changes and underlying causes of the region's climate and associated diverse ecosystem evolution during the late Quaternary. In 2015, the Towuti Drilling Project (TDP) collected a series of sedimentary drill cores from the tectonic, ferruginous, and highly biodiverse Lake Towuti, Sulawesi, one of Indonesia's oldest lakes. The drill cores contain ~1 Myr of uninterrupted lacustrine sedimentation to document long-term environmental and climatic change in the tropical western Pacific, the impacts of geological and environmental changes on the biological evolution of aquatic taxa, and the geomicrobiology and biogeochemistry of metal-rich, ultramafic-hosted lake sediment. Here we use lithostratigraphic, mineralogical, geochemical, and geochronological datasets to elucidate Lake Towuti's tectonic emergence and its biogeochemical responses to climatic and volcanic forcings since lake formation. Our data document that Lake Towuti emerged during a phase of accelerated tectonic subsidence from a landscape characterized by active river channels, shallow lakes and swamps into a permanent lake at ~1 Ma. The lacustrine sediments feature quasi-rhythmic alternations of green organic rich and red sideritic clay beds reflecting changes in lake mixing and biogeochemistry as a response to temperature and hydrological changes driven by orbital-scale changes in insolation and continental ice volume through the mid- to late Pleistocene. Clay deposition is interrupted by two beds of diatomaceous oozes composed primarily of planktonic diatoms that reflect phases of substantially increased primary productivity. The occurrence of these diatomaceous oozes in close association with multiple tephra beds suggests a trophic state change driven by the addition of volcanically sourced P, possibly in combination with a lake mixing state that supports recycling of P. Data on lake age and ontogeny are also in agreement with molecular-clock estimates of ~0.7 Ma (0.18–1.37 Ma) for the divergence of Lake Towuti's Telmatherinid fishes from a riverine ancestor. Our data therefore are compatible with an evolutionary model in which Lake Towuti's endemic fauna is a result of geographic speciation in the Malili Lakes, a set of large lakes in Southeast Sulawesi, driven by physical or chemical dispersal limits imposed by the regional rivers and lakes. More detailed chronological constraints and refined climate and environmental proxy datasets are currently in preparation and will help to paint a more detailed history of the region's climate and environmental history in future studies. © 2020 Elsevier B.V.
英文关键词	Ancient lake; Geochemistry; Paleoclimate; Paleolimnology; Sedimentology; Southeast Asia
语种	英语
scopus关键词	biogeochemistry; climate variation; diatom; dispersal; lacustrine deposit; Pleistocene; Quaternary; speciation (biology); subsidence; Far East; Greater Sunda Islands; Lake Towuti; Malili Lakes; Pacific Ocean; Pacific Ocean (West); South Sulawesi; Sulawesi; Sunda Isles; Bacillariophyta; Pisces; Telmatherinidae
来源期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/150378
作者单位	Department of Earth, Environmental, and Planetary Sciences, Brown University, 324 Brook St., Providence, RI 02912, United States; Institut of Geological Science & Oeschger Centre for Climate Change Research, University of Bern, Baltzerstrasse 1+3, Bern, 3012, Switzerland; Faculty of Mining and Petroleum Engineering, Institut Teknologi Bandung, Jalan Ganesa 10, Bandung, 40132, Indonesia; Institute for Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a/b, Cologne, 50674, Germany; Berkeley Geochronology Center, Berkeley, CA 94709, United States; Great Lakes Institute for Environmental Research, University of Windsor, Windsor, ON N9B 3P4, Canada; Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Invalidenstr. 43, Berlin, 10115, Germany; Zoological Institute, University of Basel, Vesalgasse 14051, Switzerland; School of Culture, History and Language, Australia National University, Acton, ACT 2601, Australia
推荐引用方式 GB/T 7714	Russell J.M.,Vogel H.,Bijaksana S.,et al. The late quaternary tectonic; biogeochemical; and environmental evolution of ferruginous Lake Towuti; Indonesia[J],2020,556.
APA	Russell J.M..,Vogel H..,Bijaksana S..,Melles M..,Deino A..,...&Stevenson J..(2020).The late quaternary tectonic; biogeochemical; and environmental evolution of ferruginous Lake Towuti; Indonesia.Palaeogeography, Palaeoclimatology, Palaeoecology,556.
MLA	Russell J.M.,et al."The late quaternary tectonic; biogeochemical; and environmental evolution of ferruginous Lake Towuti; Indonesia".Palaeogeography, Palaeoclimatology, Palaeoecology 556(2020).