Differential Accumulation Dynamics of Organic Matter in the Central and Eastern Bohai Bay Basin (Eastern China): Implications for Tectonic Activity. [PDF]
Li Y +10 more
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Archeological data with AI- and physics-based modeling explain typhoon-induced disasters in inland China around 3000 yr B.P. [PDF]
Ding K +18 more
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Elemental Geochemical Characteristics and Organic Matter Enrichment Model of Marine-Continental Transitional Shale in Longtan Formation, Southern Sichuan Basin. [PDF]
Gao W, Fu Y, Li H, Chen S.
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Southern Ocean influence on Atlantic Meridional Overturning Circulation across climate states. [PDF]
Song Z, Latif M, Park W, Zhang Y.
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Regime shifts of AMOC-sea surface temperature relationship. [PDF]
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PaCTS 1.0: A Crowdsourced Reporting Standard for Paleoclimate Data [PDF]
The progress of science is tied to the standardization of measurements, instruments, and data. This is especially true in the Big Data age, where analyzing large data volumes critically hinges on the data being standardized.
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Holocene Paleoclimates of India
Quaternary Research, 2006AbstractWe present a comprehensive summary of the available palaeoclimate records from India and compare the results from different proxies. The results indicate (i) fluctuating lake levels during the early Holocene. The period of relatively higher lake levels from increased precipitation efficiency was reached only ∼7.2–6.0 cal kyr BP, possibly due to
Prasad, S., Enzel, Y.
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A Global Paleoclimate Observing System
Science, 2001A major obstacle to producing reliable predictions of climate change and its impacts is a lack of data on time scales longer than the short instrumental record. Recently initiated climate observation programs will need to be continuously operated for at least 50 years before they begin to provide information that is relevant to this problem.
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The past decade saw a surge in interest in the role of the Tropics in paleoclimate changes. This was motivated by the emergence of outstanding questions in paleoclimate that pointed to a role for the Tropics in addition to advances in tropical climate dynamics. This article reviews these developments, starting from a historical perspective.
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Paleoenvironment and Paleoclimate
2015Microfossils are key to the interpretation of paleoenvironment, including the estimation of sea-level change, oceanic productivity, amount of dissolved oxygen in seawater and paleoclimate. Foraminiferal assemblages are indicators of sea-level change. The common foraminiferal genera of different depth zones on the shelf, slope and abyssal plain of the ...
Pratul Kumar Saraswati, M. S. Srinivasan
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