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A multiproxy study of past environmental changes in the Sea of Okhotsk during the last 1.5 Ma ArchiMer
Lattaud, Julie; Lo, Li; Zeeden, Christian; Liu, Ya-jun; Song, Sheng-rong; Van Der Meer, Marcel T.j.; Sinninghe Damsté, Jaap S.; Schouten, Stefan.
Long-chain diols have been detected in a wide range of environments and have been used to reconstruct past environmental changes, however only a few long-term records exist to date. Here we reconstructed past environmental changes in the central Sea of Okhotsk over the last 1.5 million years, covering the Mid-Pleistocene Transition (MPT). Sea surface temperatures (SST) reconstructed using the Long-Chain Diol Index (LDI) reflects glacial/interglacial changes. However, when compared with other organic paleothermometers (Uk’37 and TEXL86) the LDI-SST is lower during interglacials and similar or higher during glacials, possibly suggesting a shift of diol production season during interglacials. The LDI-SST does not change in periodicity around the MPT as...
Tipo: Text Palavras-chave: Sea of Okhotsk; Mid-Pleistocene Transition; LDI; TEX86; U-37(K)'; Biogenic opal; Long-chain diols.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00489/60060/63342.pdf
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Obliquity pacing of the western Pacific Intertropical Convergence Zone over the past 282,000 years ArchiMer
Liu, Yi; Lo, Li; Shi, Zhengguo; Wei, Kuo-yen; Chou, Chien-ju; Chen, Yi-chi; Chuang, Chih-kai; Wu, Chung-che; Mii, Horng-sheng; Peng, Zicheng; Amakawa, Hiroshi; Burr, George S.; Lee, Shih-yu; Delong, Kristine L.; Elderfield, Henry; Shen, Chuan-chou.
The Intertropical Convergence Zone (ITCZ) encompasses the heaviest rain belt on the Earth. Few direct long-term records, especially in the Pacific, limit our understanding of long-term natural variability for predicting future ITCZ migration. Here we present a tropical precipitation record from the Southern Hemisphere covering the past 282,000 years, inferred from a marine sedimentary sequence collected off the eastern coast of Papua New Guinea. Unlike the precession paradigm expressed in its East Asian counterpart, our record shows that the western Pacific ITCZ migration was influenced by combined precession and obliquity changes. The obliquity forcing could be primarily delivered by a cross-hemispherical thermal/pressure contrast, resulting from the...
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Ano: 2015 URL: https://archimer.ifremer.fr/doc/00334/44545/44258.pdf
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