RESEARCH PAPERModeling the East Asian Climate During the Late Cretaceous (80 Ma)
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Cited by (12)
Damp- to dry aeolian systems: Sedimentology, climate forcing, and aeolian accumulation in the Late Cretaceous Liyou Basin, South China
2021, Sedimentary GeologyCitation Excerpt :Oscillations in the water table lead to the occurrence of damp interdune facies. Previous work (Chen et al., 2009; Jiao et al., 2020; Rodríguez-López and Wu, 2020) demonstrates the influence of monsoon rainfall in the Tangbian Formation of the Xinjiang Basin, South China, suggesting a potential climate control over the phreatic water table and associated sedimentary units and structures. The aeolian succession of the Daijiaping Formation records crescentic and linear aeolian dunes.
Late Cretaceous aeolian desert system within the Mesozoic fold belt of South China: Palaeoclimatic changes and tectonic forcing of East Asian erg development and preservation
2021, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Based on a characterisation of the Late Cretaceous desert depositional system in the Xinjiang Basin, Jiao et al. (2020) suggested that water influxes into the desert basin in South China could have originated from two sources: monsoon rainfall and meltwaters from plateau mountain ranges. Although precipitation was limited in inland mid-latitude areas, monsoon rains moved northwards in summer, leading to increasing rainfall in the desert basin (see Fig. 7 in Chen et al., 2009). In addition, the supply of meltwater influxes cannot be excluded given the surrounding mountain ranges.
Late Cretaceous plateau deserts in the South China Block, and Quaternary analogues; sedimentology, dune reconstruction and wind-water interactions
2020, Marine and Petroleum GeologyCitation Excerpt :Besides, increased precipitation in the highlands recharged ground water resulting in the rise of water table in the erg system (Rodríguez-López et al., 2012a, Rodríguez-López et al., 2012b). Given that precipitation peaked along the East Asia margin during the monsoonal season while the overall precipitation is limited indicating an arid climate setting (Chen et al., 2009; Farnsworth et al., 2019), it is not likely that sudden heavy rain falls directly into the desert of Xinjiang Basin. A rise of the associated phreatic level in the aeolian erg system in the Xinjiang Basin due to increased precipitation during the monsoonal season along the East Asia margin, leading to a consequent recharge of the ground water is a plausible explanation.
Modeling East Asian climate and impacts of atmospheric CO<inf>2</inf> concentration during the Late Cretaceous (66Ma)
2013, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Their result indicates that the development of Tibetan snow and ice cover represented an additional climate feedback, which amplified the orbital forcing and produced a significant synergy with the positive vegetation feedback. Moreover, using a coupled climate system model, Chen et al. (2009a, 2009b) investigated the characteristics of East Asian climate and the effects of atmospheric CO2 concentration during the Late Cretaceous (80 Ma). It is evident that the previous studies paid little attention to simulations of East Asian climate and associated mechanisms in the Cretaceous.
"Dolomites and dolomites" in Mesozoic platform carbonates of the Southern Apennines: Geometric distribution, petrography and geochemistry
2011, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Even if the correspondence of timing of these events is still approximate, it seem reasonable that most of the dolomites of the Jurassic platforms around the Mediterranean area were formed through large-scale fluxes of seawater driven by thermal anomalies related to Tethyan spreading. The Cretaceous period is generally acknowledged as characterized by an extremely warm climate (Hallam, 1985; Frakes and Francis, 2005; Chen et al., 2009). Warm climates and geodynamics allowed carbonate platforms to spread throughout the mid-latitude shallow-water domain of Tethys from present day Mexico to the Middle East (Skelton et al., 2003).
Foundation item: Supported by the National Key Basic Research Program of China (No. 2006CB701406).