59 citations as recorded by crossref.

1. Calibrating SoilGen2 for interglacial soil evolution in the Chinese Loess Plateau considering soil parameters and the effect of dust addition rhythm K. Ranathunga et al. 10.1016/j.quaint.2021.08.019
2. Individual and combined effects of ice sheets and precession on MIS-13 climate Q. Yin et al. 10.5194/cp-5-229-2009
3. Stages of major floral change in Japan based on macrofossil evidence and their connection to climate and geomorphological changes since the Pliocene A. Momohara 10.1016/j.quaint.2015.03.008
4. Interglacial diversity P. Tzedakis et al. 10.1038/ngeo660
5. Fire history of the Chinese Loess Plateau under extreme warming scenarios: A case study of the loess-paleosol sequence L5-S5 L. Liu & S. Yang 10.1016/j.quaint.2020.09.031
6. Coupled climate-ice sheet modelling of MIS-13 reveals a sensitive Cordilleran Ice Sheet L. Niu et al. 10.1016/j.gloplacha.2021.103474
7. Progress in the reconstruction of Quaternary climate dynamics in the Northwest Pacific: A new modern analogue reference dataset and its application to the 430-kyr pollen record from Lake Biwa P. Tarasov et al. 10.1016/j.earscirev.2011.06.002
8. Time-scale and astronomical forcing of Serbian loess–paleosol sequences B. Basarin et al. 10.1016/j.gloplacha.2014.08.007
9. Magnetic monitoring of topsoil and street dust in Xinyang (China) and their environmental implications Y. Han et al. 10.1007/s10661-021-09407-1
10. Mid-Pleistocene Transition altered upper water column structure in the Bay of Bengal S. Bhadra et al. 10.1016/j.gloplacha.2023.104174
11. SST and ice sheet impacts on the MIS–13 climate H. Muri et al. 10.1007/s00382-011-1216-9
12. Strong asymmetry of hemispheric climates during MIS-13 inferred from correlating China loess and Antarctica ice records Z. Guo et al. 10.5194/cp-5-21-2009
13. Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 D. Oliveira et al. 10.1016/j.quascirev.2020.106573
14. Interglacial Hydroclimate in the Tropical West Pacific Through the Late Pleistocene A. Meckler et al. 10.1126/science.1218340
15. Climate evolution across the Mid-Brunhes Transition A. Barth et al. 10.5194/cp-14-2071-2018
16. What drives the millennial and orbital variations of δ18Oatm? A. Landais et al. 10.1016/j.quascirev.2009.07.005
17. Diverse response of global terrestrial vegetation to astronomical forcing and CO2 during the MIS-11 and MIS-13 interglacials Q. Su et al. 10.1007/s00382-022-06308-y
18. East Asian summer monsoon intensity inferred from iron oxide mineralogy in the Xiashu Loess in southern China W. Zhang et al. 10.1016/j.quascirev.2008.10.002
19. History of Asian eolian input to the West Philippine Sea over the last one million years S. Wan et al. 10.1016/j.palaeo.2012.02.015
20. Possible link of an exceptionally strong East Asian summer monsoon to a La Niña-like condition during the interglacial MIS-13 H. Lu et al. 10.1016/j.quascirev.2019.106048
21. New chronology of the best developed loess/paleosol sequence of Hungary capturing the past 1.1 ma: Implications for correlation and proposed pan-Eurasian stratigraphic schemes P. Sümegi et al. 10.1016/j.quascirev.2018.04.012
22. Middle and Late Pleistocene loess sequences at Batajnica, Vojvodina, Serbia S. Marković et al. 10.1016/j.quaint.2008.12.004
23. The Climate of the MIS-13 Interglacial according to HadCM3 H. Muri et al. 10.1175/JCLI-D-12-00520.1
24. Assessing the strength of the monsoon during the late Pleistocene in southwestern United States L. Cisneros-Dozal et al. 10.1016/j.quascirev.2014.08.022
25. Calcareous plankton and the mid-Brunhes climate variability in the Alboran Sea (ODP Site 977) M. Marino et al. 10.1016/j.palaeo.2018.07.023
26. The Eurasian ice sheet reinforces the East Asian summer monsoon during the interglacial 500 000 years ago A. Berger et al. 10.5194/cp-4-79-2008
27. A warmer but drier Marine Isotope Stage 11 during the past 650 ka as revealed by the thickest loess on the western Chinese Loess Plateau P. Shi et al. 10.1007/s40333-016-0123-7
28. Globally enhanced calcification across the coccolithophore Gephyrocapsa complex during the mid-Brunhes interval A. González-Lanchas et al. 10.1016/j.quascirev.2023.108375
29. Variability of indian monsoon and its forcing mechanisms since late quaternary L. Chen et al. 10.3389/feart.2022.977250
30. A connection between geomagnetic intensity and climatic anomalies recorded in Chinese loess J. Chen & X. Liu 10.1016/j.quaint.2015.03.016
31. A 1200 ka Stable Isotope Record From the Center of the Badain Jaran Desert, Northwestern China: Implications for the Variation and Interplay of the Westerlies and the Asian Summer Monsoon F. Wang et al. 10.1029/2020GC009575
32. Long-term cycles in the carbon reservoir of the Quaternary ocean: a perspective from the South China Sea P. Wang et al. 10.1093/nsr/nwt028
33. Records of the Mid-Brunhes Event in Chinese loess-paleosol sequences X. Xu et al. 10.1016/j.palaeo.2020.109596
34. A strong influence of the mid-Pleistocene transition on the monsoon and associated productivity in the Indian Ocean S. Bhadra & R. Saraswat 10.1016/j.quascirev.2022.107761
35. Human used upper montane ecosystem in the Horton Plains, central Sri Lanka – a link to Lateglacial and early Holocene climate and environmental changes R. Premathilake 10.1016/j.quascirev.2012.07.002
36. Impact of ice sheet induced North Atlantic oscillation on East Asian summer monsoon during an interglacial 500,000 years ago S. Sundaram et al. 10.1007/s00382-011-1213-z
37. Iron mineralogical proxies and Quaternary climate change in SE-European loess–paleosol sequences B. Buggle et al. 10.1016/j.catena.2013.06.012
38. Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model T. Caley et al. 10.1038/ncomms6371
39. High Arabian Sea productivity conditions during MIS 13 – odd monsoon event or intensified overturning circulation at the end of the Mid-Pleistocene transition? M. Ziegler et al. 10.5194/cp-6-63-2010
40. Palynological data confirm the occurrence of forest on the Loess Plateau of central China during the Middle Quaternary (MIS13) N. Wang et al. 10.1016/j.palaeo.2023.111410
41. Formation and evolution of the Badain Jaran Desert, North China, as revealed by a drill core from the desert centre and by geological survey F. Wang et al. 10.1016/j.palaeo.2015.03.011
42. Driving factors of interglacial paleosol formation on the Chinese loess plateau and the effect of precession and ice sheets K. Ranathunga et al. 10.1016/j.quascirev.2022.107911
43. Impacts of extremely asymmetrical polar ice sheets on the East Asian summer monsoon during the MIS-13 interglacial F. Shi et al. 10.1016/j.quascirev.2020.106164
44. The monsoon imprint during the ‘atypical’ MIS 13 as seen through north and equatorial Indian Ocean records T. Caley et al. 10.1016/j.yqres.2011.07.001
45. Insight into the environmental significance of grain-size fractal and pedogenesis of a typical loess and paleosol sequence K. Hou et al. 10.1016/j.catena.2022.106337
46. Pollen-based quantitative paleoclimatic record spanning the Mid-Brunhes Event in the Nihewan Basin, north China S. Da et al. 10.1016/j.palaeo.2022.111377
47. Individual contribution of insolation and CO2 to the interglacial climates of the past 800,000 years Q. Yin & A. Berger 10.1007/s00382-011-1013-5
48. Relative impact of insolation and the Indo-Pacific warm pool surface temperature on the East Asia summer monsoon during the MIS-13 interglacial Q. Yin et al. 10.5194/cp-10-1645-2014
49. Climate-soil model reveals causes of differences between Marine Isotope Stage 5e and 13 paleosols P. Finke et al. 10.1130/G39301.1
50. The last million years recorded at the Stari Slankamen (Northern Serbia) loess-palaeosol sequence: revised chronostratigraphy and long-term environmental trends S. Marković et al. 10.1016/j.quascirev.2011.02.004
51. An astronomically tuned 8.1 Ma eolian record from the Chinese Loess Plateau and its implication on the evolution of Asian monsoon W. Han et al. 10.1029/2011JD016237
52. Red palaeosols development in response to the enhanced east asia summer monsoon since the mid-pleistocene in South China: Evidence derived from magnetic properties and molecular fossil records Y. Gu et al. 10.1007/s12583-013-0331-4
53. State of the tropical Pacific Ocean and its enhanced impact on precipitation over East Asia during marine isotopic stage 13 M. Karami et al. 10.1007/s00382-014-2227-0
54. Reply to comment by Riccardo Caputo and Marcello Bianca on “Late Cenozoic uplift of southern Italy deduced from fluvial and marine sediments: Coupling between surface processes and lower-crustal flow” by Rob Westaway and David Bridgland; improved uplift modelling of the Gulf of Taranto marine terraces R. Westaway & D. Bridgland 10.1016/j.quaint.2009.09.012
55. Stratigraphic distribution of the radiolarian Spongodiscus biconcavus Haeckel at IODP Site U1340 in the Bering Sea and its paleoceanographic significance M. Chen et al. 10.1016/j.palwor.2013.11.001
56. Stable oxygen and carbon isotope record from a drill core from the Hetao Basin in the upper reaches of the Yellow River in northern China and its implications for paleolake evolution B. Li et al. 10.1016/j.chemgeo.2020.119798
57. The global monsoon across timescales: coherent variability of regional monsoons P. Wang et al. 10.5194/cp-10-2007-2014
58. Influence of tectonic uplift of the Qinling Mountains on the paleoclimatic environment of surrounding areas: Insights from loess–paleosol sequences, Weihe Basin, central China K. Hou et al. 10.1016/j.catena.2019.104336
59. Ancient east-west divergence, recent admixture, and multiple marginal refugia shape genetic structure of a widespread oak species (Quercus acutissima) in China X. Zhang et al. 10.1007/s11295-018-1302-9