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Li et al. ( 2017) precipitation data from Gonghai Lake is available through Chen et al. ( 2015) integrated ISM proxy based on four cave δ 18O records (Sahiya, Hoti, Mawmluh, and Qunf) is available through X. ( 2011) and Zheng et al. ( 2014) the fossil pollen assemblage from Qinghai Lake is available through Liu et al. ( 2002) precipitation data from Qinghai Lake in Figure 3c are available through Herzschuh et al. ( 2010) and J. Modern pollen calibration dateset is available through Xu et al., ( 2010) Lu, Wu, et al. Key Pointsĭata generated by this study are available at the Figshare website ( ). Our well-dated and unambiguous P ann record also provides the opportunity to reconcile paleoenvironmental reconstructions derived from different paleoenvironmental proxies from the Qinghai Lake basin. We propose that the pattern of precipitation evolution in the Qinghai Lake basin resulted from the combined effects of the ISM and EASM, with a precipitation maximum of 10–7 ka for the ISM and 7–5 ka for the EASM both systems contributed to the regional precipitation maximum during 10–5 ka. A synthesis of the P ann records from the two sites indicates that the precipitation in the region began to increase before 10 ka, reached a maximum during 10–5 ka, and gradually decreased thereafter. The results suggest that mean annual precipitation (P ann) is the most significant factor controlling the fossil pollen record at both sites, and the P ann reconstructions are well correlated with each other ( r = 0.72, p < 0.001). In addition, we use a novel procedure for pollen-based quantitative paleoclimatic reconstruction to characterize the evolution of precipitation at Caodalian Lake and nearby Qinghai Lake.
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Here we present a high-resolution pollen record from Caodalian Lake since 7.9 ka (1 ka = 1,000 cal yr BP), which is used to reconstruct the regional vegetation history and climatic changes. However, how these various circulation systems interacted in the region during the Holocene, and the nature of the associated environmental impacts, are unclear and even controversial. Continued abuse of our services will cause your IP address to be blocked indefinitely.The northeastern Qinghai-Tibet Plateau is strongly influenced by the East Asian summer monsoon (EASM), the Indian summer monsoon (ISM) and the westerlies. Please fill out the CAPTCHA below and then click the button to indicate that you agree to these terms. If you wish to be unblocked, you must agree that you will take immediate steps to rectify this issue. If you do not understand what is causing this behavior, please contact us here. If you promise to stop (by clicking the Agree button below), we'll unblock your connection for now, but we will immediately re-block it if we detect additional bad behavior. Overusing our search engine with a very large number of searches in a very short amount of time.Using a badly configured (or badly written) browser add-on for blocking content.Running a "scraper" or "downloader" program that either does not identify itself or uses fake headers to elude detection.Using a script or add-on that scans GameFAQs for box and screen images (such as an emulator front-end), while overloading our search engine.There is no official GameFAQs app, and we do not support nor have any contact with the makers of these unofficial apps. Continued use of these apps may cause your IP to be blocked indefinitely.
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