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• W2766707988 endingPage "302" @default.
• W2766707988 startingPage "287" @default.
• W2766707988 abstract "Abstract. The climate during the Cretaceous Period represented one of the greenhouse states of Earth's history. Significant transformation of climate patterns and a mass extinction event characterised by the disappearance of dinosaurs occurred across the Cretaceous–Palaeogene boundary. However, most records of this interval are derived from marine sediments. The continuous and well-exposed red strata of the Nanxiong Basin (SE China) provide ideal material to develop continental records. Considerable research into stratigraphic, palaeontological, chronologic, palaeoclimatic, and tectonic aspects has been carried out for the Datang profile, which is a type section of a non-marine Cretaceous–Palaeogene stratigraphic division in China. For this study, we reviewed previous work and found that (1) the existing chronological framework of the Datang profile is flawed; (2) precise palaeoclimatic reconstruction is lacking because of the limitations of sampling resolution (e.g. carbonate samples) and/or the lack of efficient proxies; and (3) comparisons of climate changes between marine and continental records are lacking. To resolve these problems, detailed field observations and sampling, as well as environmental magnetic and rare earth element (REE) measurements, were carried out. The results show that (1) more accurate ages of the Datang profile range from 72 to 62.8 Ma based on a combination of the most recently published radiometric, palaeontological, and palaeomagnetic ages; (2) there is considerable evidence of palaeosol generation, which indicates that the red strata formed in a long-term hot, oxidising environment that lacked underwater conditions; (3) haematite was the dominant magnetic mineral in the red strata, and the variation trend of magnetic susceptibility was consistent with the oxygen isotope records from deep-sea sediments, which indicates that the content of haematite was controlled by the global climate; and (4) the palaeoclimate changes from 72 to 62.8 Ma in the Nanxiong Basin were consistent with global patterns and can be divided into three stages: a relatively hot and wet stage during 72–71.5 Ma, a cool and arid stage during 71.5–66 Ma, and a relatively hot and wet stage again during 66–62.8 Ma with a notable drying and cooling event at 64.7–63.4 Ma. Moreover, there are several sub-fluctuations during each stage. This work provides basic information for further palaeoclimate reconstructions with a higher resolution and longer timescales for the Cretaceous to Palaeocene in the Nanxiong Basin and may even help to test ocean–land climate interactions in the future." @default.
• W2766707988 created "2017-11-10" @default.
• W2766707988 creator A5003635871 @default.
• W2766707988 creator A5061949925 @default.
• W2766707988 creator A5076112088 @default.
• W2766707988 date "2018-03-08" @default.
• W2766707988 modified "2023-10-13" @default.
• W2766707988 title "Palaeoclimate evolution across the Cretaceous–Palaeogene boundary in the Nanxiong Basin (SE China) recorded by red strata and its correlation with marine records" @default.
• W2766707988 cites W10666912 @default.
• W2766707988 cites W1473370317 @default.
• W2766707988 cites W1840659500 @default.
• W2766707988 cites W1908932275 @default.
• W2766707988 cites W1927390709 @default.
• W2766707988 cites W1955302243 @default.
• W2766707988 cites W1964523361 @default.
• W2766707988 cites W1968346323 @default.
• W2766707988 cites W1969933645 @default.
• W2766707988 cites W1972047036 @default.
• W2766707988 cites W1972289403 @default.
• W2766707988 cites W1977307052 @default.
• W2766707988 cites W1978868361 @default.
• W2766707988 cites W1979215745 @default.
• W2766707988 cites W1981605974 @default.
• W2766707988 cites W1985923587 @default.
• W2766707988 cites W1987593072 @default.
• W2766707988 cites W1988249033 @default.
• W2766707988 cites W1991908329 @default.
• W2766707988 cites W1992771347 @default.
• W2766707988 cites W1992974292 @default.
• W2766707988 cites W1994473632 @default.
• W2766707988 cites W1999206191 @default.
• W2766707988 cites W1999359470 @default.
• W2766707988 cites W2003879650 @default.
• W2766707988 cites W2009979849 @default.
• W2766707988 cites W2013306572 @default.
• W2766707988 cites W2016116453 @default.
• W2766707988 cites W2016754172 @default.
• W2766707988 cites W2018552304 @default.
• W2766707988 cites W2018773796 @default.
• W2766707988 cites W2020224198 @default.
• W2766707988 cites W2020986930 @default.
• W2766707988 cites W2025360819 @default.
• W2766707988 cites W2026685721 @default.
• W2766707988 cites W2028923623 @default.
• W2766707988 cites W2036189008 @default.
• W2766707988 cites W2039349517 @default.
• W2766707988 cites W2039539573 @default.
• W2766707988 cites W2041513053 @default.
• W2766707988 cites W2047514309 @default.
• W2766707988 cites W2047741499 @default.
• W2766707988 cites W2049696180 @default.
• W2766707988 cites W2049793461 @default.
• W2766707988 cites W2059434190 @default.
• W2766707988 cites W2060527284 @default.
• W2766707988 cites W2061952742 @default.
• W2766707988 cites W2064835792 @default.
• W2766707988 cites W2066770188 @default.
• W2766707988 cites W2072263363 @default.
• W2766707988 cites W2073415607 @default.
• W2766707988 cites W2076468359 @default.
• W2766707988 cites W2077053821 @default.
• W2766707988 cites W2077538534 @default.
• W2766707988 cites W2078992693 @default.
• W2766707988 cites W2080572512 @default.
• W2766707988 cites W2087135514 @default.
• W2766707988 cites W2088701426 @default.
• W2766707988 cites W2089400264 @default.
• W2766707988 cites W2093636601 @default.
• W2766707988 cites W2095197054 @default.
• W2766707988 cites W2096766635 @default.
• W2766707988 cites W2098187169 @default.
• W2766707988 cites W2100044125 @default.
• W2766707988 cites W2100421952 @default.
• W2766707988 cites W2104821529 @default.
• W2766707988 cites W2105190152 @default.
• W2766707988 cites W2109482546 @default.
• W2766707988 cites W2115575384 @default.
• W2766707988 cites W2123306717 @default.
• W2766707988 cites W2123815181 @default.
• W2766707988 cites W2124272991 @default.
• W2766707988 cites W2129165799 @default.
• W2766707988 cites W2131733332 @default.
• W2766707988 cites W2143218087 @default.
• W2766707988 cites W2143505127 @default.
• W2766707988 cites W2146152064 @default.
• W2766707988 cites W2151613397 @default.
• W2766707988 cites W2154501314 @default.
• W2766707988 cites W2154973565 @default.
• W2766707988 cites W2155427977 @default.
• W2766707988 cites W2165876571 @default.
• W2766707988 cites W2176312582 @default.
• W2766707988 cites W2274986068 @default.
• W2766707988 cites W2316455897 @default.
• W2766707988 cites W2316608501 @default.
• W2766707988 cites W2318001326 @default.
• W2766707988 cites W2332439330 @default.
• W2766707988 cites W2372909365 @default.
• W2766707988 cites W2555568769 @default.

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