Multidisciplinary and Interdisciplinary(M) | ||
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Session Sub-category | Intersection | |
Session ID | M-IS01 | |
Related Fields | A, H, S, B | |
Title | Evolution and variability of Asian Monsoon and its linkage with Cenozoic global cooling | |
Short Title | Evolution of Asian Monsoon | |
Main Convener | Name | Masanobu Yamamoto |
Affiliation | Faculty of Environmental Earth Science, Hokkaido University | |
Co-Convener 1 | Name | Ryuji Tada |
Affiliation | Department of Earth and Planetary Science, Graduate School of Science, The Univeristy of Tokyo | |
Session Language | EE | |
Scope | Although Asian Monsoon (AM) is a regional phenomenon, it exerts a significant impact on the global climate. Since uplift of Himalaya and Tibetan Plateau (HTP) has been considered to have played a significant role on the establishment and intensification of AM, numerous attempts have been made to prove the linkage between the HTP uplift and AM evolution, but the linkage is largely unproved till now. On the other hand, comparison of global climatic changes, pCO2 reconstructions, and AM evolution process during Cenozoic suggests that AM evolution is significantly affected by global climate changes most likely through pCO2. Thus, importance of the HTP uplift on AM evolution is questioned. However, it should be noted that the effects of the HTP uplift and AM precipitation on chemical weathering, erosion, and CO2 uptake could be acting as feedback loops on AM-HTP uplift linkage. From July 2013 to November 2016, IODP conducted a series of expeditions such as 346 (Asian Monsoon), 353 (Indian Monsoon Rainfall), 354 (Bengal Fan), 355 (Arabian Monsoon), 356 (Indian through-flow), and 359 (Maldives Monsoon) that are related to AM evolution and its interaction with global climate system in NW Pacific and Indian Ocean regions, and exciting results are gradually coming out. We believe it is timely to start gathering and synthesizing the results of these cruises and update and exchange information and ideas to promote our understanding of AM evolution, variability, their controlling factors, and their interaction with global climate system during the Cenozoic. | |
Presentation Format | Oral and Poster presentation | |
Joint Session with | AGU | |
Co-Sponsoring Societies (Society Members) | PALEO10: Paleosciences Society | |
Invited Authors |
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Time | Presentation No | Title | Presenter | Abstract |
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Oral Presentation May 21 PM1 | ||||
13:45 - 14:00 | MIS01-01 | Distinctly light layers in the Quaternary sediments of the Japan Sea as a possible indicator of millennial-scale variability of East Asian winter monsoon | Ryuji Tada | Abstract |
14:00 - 14:20 | MIS01-02 | Precession-band variance missing from East Asian monsoon runoff | Steven C Clemens | Abstract |
14:20 - 14:35 | MIS01-03 | The Eccentricity cycle forcing (100 & 400 kyr) during the late Miocene in the Japan Sea and its impact of the local paleoceanography, evidence from data of radiolarians and sediment physical properties (IODP Expedition 346 Site U1425) | Kenji Marc Raymond Matsuzaki | Abstract |
14:35 - 14:55 | MIS01-04 | Indian monsoon variability in a warmer world: Exploring IODP Expedition 353 Miocene sediment archives | Wolfgang Kuhnt | Abstract |
14:55 - 15:15 | MIS01-05 | Sensitivity of Australian monsoon to changing climate boundary conditions during the late Miocene and across the Mid-Pleistocene Transition | Ann E Holbourn | Abstract |
Oral Presentation May 21 PM2 | ||||
15:30 - 15:45 | MIS01-06 | Asia dust production ramped up since latest Oligocene: Tibetan Plateau uplift vs global cooling | Hongbo Zheng | Abstract |
15:45 - 16:00 | MIS01-07 | Provenance changes of dust in the sediments of the Japan Sea associated with westerly jet shifts since 5 Ma. | Ke WANG | Abstract |
16:00 - 16:15 | MIS01-08 | Relationship between typhoon-induced hazards in East Asia, pressure and SST pattern in Pacific Ocean during the Middle to Late Holocene | Yoshiaki Suzuki | Abstract |
16:15 - 16:30 | MIS01-09 | Paleoecological variations in marine producers of the Andaman Sea during the late Miocene reconstructed by algal biomarkers in sediments from site U1447 (Exp. 353) | Takuto Ando | Abstract |
16:30 - 16:45 | MIS01-10 | History of the Leeuwin Current during the last 5 million years: Evidence from seawater Neodymium isotope variation | Hideko Takayanagi | Abstract |
16:45 - 17:00 | MIS01-11 | Miocene aridity and sabkha development: Southeast Indian Ocean offshore western Australia | Cecilia M McHugh | Abstract |
Presentation No | Title | Presenter | Abstract |
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Poster Presentation May 21 Core Time | |||
MIS01-P01 | Reconstruction of Asian dust source variability since 10 Ma based on grain size specific mineral composition at IODP Site U1425 in the Japan Sea | Mui Fa Alison Lee | Abstract |
MIS01-P02 | Two step expansion of C4 plants in northwestern India at 10 Ma and 7.5 Ma: Evidence of leaf wax carbon isotopes in IODP Site U1457 sediments | Masanobu Yamamoto | Abstract |
MIS01-P03 | Changes in provenance and chemical weathering of Cenozoic fluvial sediments in the southwestern margin of Tarim Basin deduced from their mineral and chemical compositions | Tomohiro Kanzaki | Abstract |
MIS01-P04 | Biomass burning history and possible origin of fire in East Asia during the million years using chemical proxies | Song Lu | Abstract |
MIS01-P05 | Provenance changes of the Cenozoic terrestrial sequence in the southwestern Tarim basin and its implication to tectonics of the source area | Aki Sakuma | Abstract |
MIS01-P06 | Application of cellulose oxygen isotopes in sphagunum from the Bekanbeushi mire, eastern Hokkaido to the reconstruction of“Ezo-tsuyu”and the East Asian summer monsoon during the last 2000 years. | Hiromichi Sakurai | Abstract |