49 citations as recorded by crossref.

1. Individual and combined effects of ice sheets and precession on MIS-13 climate Q. Yin et al. 10.5194/cp-5-229-2009
2. 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
3. Interglacial diversity P. Tzedakis et al. 10.1038/ngeo660
4. 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
5. Coupled climate-ice sheet modelling of MIS-13 reveals a sensitive Cordilleran Ice Sheet L. Niu et al. 10.1016/j.gloplacha.2021.103474
6. 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
7. Time-scale and astronomical forcing of Serbian loess–paleosol sequences B. Basarin et al. 10.1016/j.gloplacha.2014.08.007
8. SST and ice sheet impacts on the MIS–13 climate H. Muri et al. 10.1007/s00382-011-1216-9
9. 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
10. 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
11. Interglacial Hydroclimate in the Tropical West Pacific Through the Late Pleistocene A. Meckler et al. 10.1126/science.1218340
12. Climate evolution across the Mid-Brunhes Transition A. Barth et al. 10.5194/cp-14-2071-2018
13. What drives the millennial and orbital variations of δ18Oatm? A. Landais et al. 10.1016/j.quascirev.2009.07.005
14. 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
15. 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
16. 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
17. 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
18. Middle and Late Pleistocene loess sequences at Batajnica, Vojvodina, Serbia S. Marković et al. 10.1016/j.quaint.2008.12.004
19. The Climate of the MIS-13 Interglacial according to HadCM3 H. Muri et al. 10.1175/JCLI-D-12-00520.1
20. 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
21. 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
22. 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
23. 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
24. A connection between geomagnetic intensity and climatic anomalies recorded in Chinese loess J. Chen & X. Liu 10.1016/j.quaint.2015.03.016
25. 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
26. 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
27. Records of the Mid-Brunhes Event in Chinese loess-paleosol sequences X. Xu et al. 10.1016/j.palaeo.2020.109596
28. 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
29. 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
30. Iron mineralogical proxies and Quaternary climate change in SE-European loess–paleosol sequences B. Buggle et al. 10.1016/j.catena.2013.06.012
31. 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
32. 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
33. 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
34. 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
35. 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
36. 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
37. Climate-soil model reveals causes of differences between Marine Isotope Stage 5e and 13 paleosols P. Finke et al. 10.1130/G39301.1
38. 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
39. 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
40. 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
41. 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
42. 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
43. 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
44. 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
45. The global monsoon across timescales: coherent variability of regional monsoons P. Wang et al. 10.5194/cp-10-2007-2014
46. 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
47. Orbital-scale evolution of the Indian summer monsoon since 1.2 Ma: Evidence from clay mineral records at IODP Expedition 355 Site U1456 in the eastern Arabian Sea H. Chen et al. 10.1016/j.jseaes.2018.10.012
48. 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
49. Iberian Margin sea surface temperature during MIS 15 to 9 (580–300 ka): Glacial suborbital variability versus interglacial stability T. Rodrigues et al. 10.1029/2010PA001927