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• W1994930768 abstract "To explore the evolution of climate through the Miocene, especially during the Middle Miocene climate transition, multiproxy continental records were analyzed by susceptibility (SUS), lightness (L⁎), total inorganic carbon (TIC) and total organic carbon (TOC) content from the 2900-m-thick fluviolacustrine sediment sequence at Guyuan, Ningxia, China and compared with the redness (a⁎) and the pollen humidity indices from the same section. The published Miocene records of sedimentation rate, sediment grain size, biota turnover, and palaeoproductivity from other regions were also compiled and compared. Results show that multiproxies of the Sikouzi section have changed substantially since 12–11 Ma ago. SUS, L⁎ and TIC have increased while a⁎, TOC and the pollen humidity index decreased, all implying that the palaeoclimate in the study area has got cooler and drier since that time. This climate change also left imprints in many other regions, probably resulting from global cooling and the development of the East Antarctic Ice Sheet since about 14 Ma. Several positive feedback mechanisms are proposed to have effectively modulated and magnified the Mid-Miocene global cooling, including vegetation change, greenhouse gas (atmospheric CO2 and water vapor) fluctuations. They led to the strengthing of ocean and atmospheric circulation, significant lowering of sea level and increasing aridification over the globe, especially in middle-high latitudes. Since 12–11 Ma ago, a continuously cooler and drier climate may have caused the substantial intensification of physical weathering and exhumation on the earth's surface, the increased sediment accumulation rates on the land and in the sea, and the inception of productivity increase in the oceans. Nevertheless, when and where these mechanisms operated and how they were tied to each other remain ambiguous, deserving further investigation." @default.
• W1994930768 created "2016-06-24" @default.
• W1994930768 creator A5004466460 @default.
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• W1994930768 creator A5036811526 @default.
• W1994930768 date "2008-07-01" @default.
• W1994930768 modified "2023-10-13" @default.
• W1994930768 title "Cooling-driven climate change at 12–11 Ma: Multiproxy records from a long fluviolacustrine sequence at Guyuan, Ningxia, China" @default.
• W1994930768 cites W1525484356 @default.
• W1994930768 cites W1539328855 @default.
• W1994930768 cites W1601117563 @default.
• W1994930768 cites W1923703724 @default.
• W1994930768 cites W1964500653 @default.
• W1994930768 cites W1964765493 @default.
• W1994930768 cites W1964979838 @default.
• W1994930768 cites W1965324527 @default.
• W1994930768 cites W1965547181 @default.
• W1994930768 cites W1965840594 @default.
• W1994930768 cites W1968833157 @default.
• W1994930768 cites W1972685338 @default.
• W1994930768 cites W1972694007 @default.
• W1994930768 cites W1974103614 @default.
• W1994930768 cites W1976156138 @default.
• W1994930768 cites W1977383913 @default.
• W1994930768 cites W1982903817 @default.
• W1994930768 cites W1985195204 @default.
• W1994930768 cites W1992967062 @default.
• W1994930768 cites W1997252211 @default.
• W1994930768 cites W1997655520 @default.
• W1994930768 cites W1998563399 @default.
• W1994930768 cites W1998909488 @default.
• W1994930768 cites W1999538456 @default.
• W1994930768 cites W2000586618 @default.
• W1994930768 cites W2004288509 @default.
• W1994930768 cites W2004714190 @default.
• W1994930768 cites W2005228122 @default.
• W1994930768 cites W2005992151 @default.
• W1994930768 cites W2008622484 @default.
• W1994930768 cites W2010164667 @default.
• W1994930768 cites W2012934898 @default.
• W1994930768 cites W2013437810 @default.
• W1994930768 cites W2013752202 @default.
• W1994930768 cites W2014567053 @default.
• W1994930768 cites W2015172189 @default.
• W1994930768 cites W2016581298 @default.
• W1994930768 cites W2017048129 @default.
• W1994930768 cites W2022069268 @default.
• W1994930768 cites W2026252331 @default.
• W1994930768 cites W2026708294 @default.
• W1994930768 cites W2028710503 @default.
• W1994930768 cites W2035980065 @default.
• W1994930768 cites W2040146427 @default.
• W1994930768 cites W2043333517 @default.
• W1994930768 cites W2046171913 @default.
• W1994930768 cites W2049177412 @default.
• W1994930768 cites W2049696180 @default.
• W1994930768 cites W2053668010 @default.
• W1994930768 cites W2054410655 @default.
• W1994930768 cites W2055792591 @default.
• W1994930768 cites W2058164319 @default.
• W1994930768 cites W2062552134 @default.
• W1994930768 cites W2063916634 @default.
• W1994930768 cites W2064205665 @default.
• W1994930768 cites W2064803191 @default.
• W1994930768 cites W2065078273 @default.
• W1994930768 cites W2067990228 @default.
• W1994930768 cites W2069631000 @default.
• W1994930768 cites W2070511571 @default.
• W1994930768 cites W2072504982 @default.
• W1994930768 cites W2074893072 @default.
• W1994930768 cites W2084579279 @default.
• W1994930768 cites W2085677570 @default.
• W1994930768 cites W2089827533 @default.
• W1994930768 cites W2093636601 @default.
• W1994930768 cites W2096649360 @default.
• W1994930768 cites W2107137304 @default.
• W1994930768 cites W2108316127 @default.
• W1994930768 cites W2109417453 @default.
• W1994930768 cites W2115575384 @default.
• W1994930768 cites W2118627997 @default.
• W1994930768 cites W2135051776 @default.
• W1994930768 cites W2138799022 @default.
• W1994930768 cites W2143000529 @default.
• W1994930768 cites W2152377052 @default.
• W1994930768 cites W2158746766 @default.
• W1994930768 cites W2165473271 @default.
• W1994930768 cites W2175785056 @default.
• W1994930768 doi "https://doi.org/10.1016/j.palaeo.2008.05.006" @default.
• W1994930768 hasPublicationYear "2008" @default.
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