Kalimantan hydroclimate variability since the last glacial period

被引:1
作者
Hendrizan, Marfasran [1 ,2 ,3 ]
Kuhnt, Wolfgang [2 ]
Holbourn, Ann [2 ]
Cahyarini, Sri Yudawati [3 ]
Ningsih, Nining Sari [4 ]
机构
[1] Inst Teknol Bandung, Fac Earth Sci & Technol, Doctoral Program Earth Sci, Labtek 11,Jl Ganesha 10, Bandung 40132, Jawa Barat, Indonesia
[2] Univ Kiel, Inst Geosci, Ludewig Meyn Str 10, D-24118 Schleswig, Schleswig Holst, Germany
[3] Natl Res & Innovat Agcy Republ Indonesia BRIN, Res Org Earth Sci & Maritime, Res Ctr Climate & Atmosphere, Paleoclimate & Paleoenvironm Res Grp, Jl Sangkuriang, Bandung 40135, Jawa Barat, Indonesia
[4] Inst Teknol Bandung, Fac Earth Sci & Technol, Res Grp Oceanog, Labtek 11,Jl. Ganesha 10, Bandung 40132, Jawa Barat, Indonesia
关键词
Hydroclimate; Sediment discharge; Holocene; Late Pleistocene; Northeastern Kalimantan; Makassar Strait; INDONESIAN THROUGHFLOW; THERMOCLINE STRUCTURE; SEDIMENT LOAD; TAYLOR-DOME; HOLOCENE; CLIMATE; SEA; BORNEO; VEGETATION; HYDROLOGY;
D O I
10.1007/s00531-022-02266-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Changes in convective activity and hydroclimate over Northeastern Kalimantan are key features to understand glacial to interglacial climate evolution in the center of the West Pacific Warm Pool during the Late Pleistocene to Holocene. We use high-resolution X-ray fluorescence (XRF) scanner-derived elemental ratios in sediment Core SO217-18522 (1o 24.106' N, 119o 4.701'E, 975 m water depth) recovered from the northern Makassar Strait to reconstruct changes in precipitation-related weathering and erosion over Northeastern Kalimantan over the last 50 kyr. Enhanced seasonality of rainfall and an extended dry season during Heinrich Stadials (HS4 to HS1) and the Younger Dryas (YD) suggest weakening of the tropical convection associated with a southward shift of the tropical rain belt and the annual mean position of the Intertropical Tropical Convection Zone. Increasing sediment discharge and intensification of convective activity occurred during the early to mid-Holocene during an interval of high Northern Hemisphere insolation, elevated atmospheric pCO(2) levels and global warming. Our reconstructions in comparison with regional terrestrial and marine records highlight the high spatial variability of Kalimantan hydroclimate on millennial to glacial-interglacial timescales.
引用
收藏
页码:615 / 629
页数:15
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