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- W2351567252 abstract "An important goal of palaeoclimatology is to understand how the land and ocean are coupled during climate changes. Most of studies in paleoclimatology has oriented towards determining the relative timing of climate events, particularly the rapid climate change events that represented the last glacial period, in different parts of the globe or in different climate subsystems. Unfortunately, detailed knowledge concerning leads or lags of climate changes between land and sea on the millennial time scale is still lacking. Here we present new high-resolution records of four proxies, including marine, foraminifera, pollen, and phytolith, from the same core DG9603 located at the Okinawa Trough, East China Sea (ECS), providing a continuous and directly linked evidence for the processes of marine and terrestrial climate changes. The data show that during the last 20 ka oceanographic changes of the ECS lagged behind the epicontinent climate changes by about 1 000 a. We suggest that the thermohaline circulation, being a potential thermal source of long-term memory on time scales up to a millennium, was the major driving factor for asynchronous changes between marine and continental climatic systems in East Asia." @default.
- W2351567252 created "2016-06-24" @default.
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- W2351567252 date "2002-01-01" @default.
- W2351567252 modified "2023-09-25" @default.
- W2351567252 title "ASYNCHRONY OF THE MARINE AND EPICONTINENTAL CLIMATE RECORDS IN THE EAST ASIA DURING THE LAST 20 ka" @default.
- W2351567252 hasPublicationYear "2002" @default.
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