Orbitally and galactic cosmic forced abrupt climate events during the last glacial period

[1]  S. Wan,et al.  Tectonic and Climatic Impacts on Environmental Evolution in East Asia During the Palaeogene , 2021, Geophysical Research Letters.

[2]  S. Clemens,et al.  Persistent orbital influence on millennial climate variability through the Pleistocene , 2021, Nature Geoscience.

[3]  A. Berger,et al.  Insolation triggered abrupt weakening of Atlantic circulation at the end of interglacials , 2021, Science.

[4]  M. Crucifix,et al.  Diverse Regional Sensitivity of Summer Precipitation in East Asia to Ice Volume, CO2 and Astronomical Forcing , 2021, Geophysical Research Letters.

[5]  J. Russell,et al.  A global environmental crisis 42,000 years ago , 2021, Science.

[6]  L. Vigliotti,et al.  The Role of Geomagnetic Field Intensity in Late Quaternary Evolution of Humans and Large Mammals , 2019, Reviews of Geophysics.

[7]  Frank Oldfield,et al.  The different climatic response of pedogenic hematite and ferrimagnetic minerals: Evidence from particle-sized modern soils over the Chinese Loess Plateau , 2017 .

[8]  Gaozhong Nie,et al.  A continuous 13.3-ka record of seismogenic dust events in lacustrine sediments in the eastern Tibetan Plateau , 2017, Scientific Reports.

[9]  H. Synal,et al.  An improved north–south synchronization of ice core records around the 41 kyr 10 Be peak , 2017 .

[10]  J. Bassis,et al.  Heinrich events triggered by ocean forcing and modulated by isostatic adjustment , 2017, Nature.

[11]  J. McManus,et al.  North Atlantic ocean circulation and abrupt climate change during the last glaciation , 2016, Science.

[12]  R. Edwards,et al.  The Asian monsoon over the past 640,000 years and ice age terminations , 2016, Nature.

[13]  J. Seinfeld,et al.  Ion-induced nucleation of pure biogenic particles , 2016, Nature.

[14]  I. Suter,et al.  Impact of geomagnetic excursions on atmospheric chemistry and dynamics , 2014 .

[15]  C. Laj,et al.  Dynamics of the earth magnetic field in the 10-75 kyr period comprising the Laschamp and Mono Lake excursions: New results from the French Chaîne des Puys in a global perspective , 2014 .

[16]  M. Caffee,et al.  Timing and climatic drivers for glaciation across semi-arid western Himalayan–Tibetan orogen , 2013 .

[17]  F. Parrenin,et al.  The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years , 2012 .

[18]  Huayu Lu,et al.  The ultrafine component in Chinese loess and its variation over the past 7·6 Ma: implications for the history of pedogenesis , 2011 .

[19]  A. Tani,et al.  Millennial-scale oscillations of the westerly jet path during the last glacial period , 2011 .

[20]  Jessica A. Thompson,et al.  Last glacial pollen record from Lanzhou (Northwestern China) and possible forcing mechanisms for the MIS 3 climate change in Middle to East Asia , 2011 .

[21]  P. Kubik,et al.  Early last glacial maximum in the southern Central Andes reveals northward shift of the westerlies at ~39 ka , 2010 .

[22]  M. Loutre,et al.  Total irradiation during any time interval of the year using elliptic integrals , 2010 .

[23]  Bin Zhang,et al.  Optically stimulated luminescence dating of sediments from the Yellow River terraces in Lanzhou: Tectonic and climatic implications , 2010 .

[24]  Jessica A. Thompson,et al.  Last glacial climate instability documented by coarse-grained sediments within the loess sequence, at Fanjiaping, Lanzhou, China , 2009, Quaternary Research.

[25]  Xiaohua Shao,et al.  Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years , 2008, Nature.

[26]  A. Wintle,et al.  A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau , 2007, Quaternary Research.

[27]  M. Loutre,et al.  Equatorial insolation: from precession harmonics to eccentricity frequencies , 2006 .

[28]  R. Edwards,et al.  High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China , 2006 .

[29]  Jimin Sun,et al.  Half-precessional cycles recorded in Chinese loess: response to low-latitude insolation forcing during the Last Interglaciation , 2006 .

[30]  J. Kirkby.  Cosmic Rays and Climate , 2005, 0804.1938.

[31]  N. Mahowald,et al.  Global Iron Connections Between Desert Dust, Ocean Biogeochemistry, and Climate , 2005, Science.

[32]  T. Delworth,et al.  Simulated Tropical Response to a Substantial Weakening of the Atlantic Thermohaline Circulation , 2005 .

[33]  S. Hemming,et al.  Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint , 2004 .

[34]  J. Overpeck,et al.  Abrupt Climate Change , 2003, Science.

[35]  R. L. Edwards,et al.  A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China , 2001, Science.

[36]  D. Livingstone,et al.  Some results relevant to the discussion of a possible link between cosmic rays and the Earth's climate , 2001 .

[37]  Stefan Rahmstorf,et al.  Rapid changes of glacial climate simulated in a coupled climate model , 2001, Nature.

[38]  Z. Ding,et al.  Climate instability during the penultimate glaciation: Evidence from two high‐resolution loess records, China , 1999 .

[39]  Yongxin Pan,et al.  Geomagnetic excursions recorded in Chinese Loess in the last 70,000 years , 1999 .

[40]  Z. Ding,et al.  CHINESE LOESS AND THE PALEOMONSOON , 1998 .

[41]  A. Hunt,et al.  Possible triggering of Heinrich events by ice-load-induced earthquakes , 1998, Nature.

[42]  Scott J. Lehman,et al.  Suborbital timescale variability of North Atlantic Deep Water during the past 200 , 1995 .

[43]  A. Zhisheng,et al.  Correlation between climate events in the North Atlantic and China during the last glaciation , 1995, Nature.

[44]  J. Prescott,et al.  Cosmic ray contributions to dose rates for luminescence and ESR dating: Large depths and long-term time variations , 1994 .

[45]  H. Heinrich,et al.  Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years , 1988, Quaternary Research.

[46]  D. Schulze,et al.  Is there holocene reddening (hematite formation) in soils of axeric temperate areas , 1982 .

[47]  R. Dickinson.  Solar variability and the lower atmosphere. , 1975 .

[48]  R. Passega.  Grain size representation by CM patterns as a geologic tool , 1964 .

[49]  Basanta K. Sahu,et al.  Depositional mechanisms from the size analysis of clastic sediments , 1964 .

[50]  Hongyan Xu,et al.  Provenance and earthquake signature of the last deglacial Xinmocun lacustrine sediments at Diexi, East Tibet , 2014 .

[51]  S. Clemens,et al.  Influence of Atlantic meridional overturning circulation on the East Asian winter monsoon , 2012 .

[52]  Yan-chou Lu,et al.  On the performances of the single-aliquot regenerative-dose (SAR) protocol for Chinese loess: fine quartz and polymineral grains , 2006 .

[53]  L. Tiegang,et al.  The paleoclimatic change since the last glaciation in the north of Okinawa Trough based on the spore-pollen records , 2006 .

[54]  Zhongli Ding,et al.  Temporal and spatial changes of vegetation cover on the Chinese Loess Plateau through the last glacial cycle: evidence from spore-pollen records , 2005 .

[55]  M. Sharma,et al.  Quaternary glacial history of NW Garhwal, Central himalayas , 1996 .

[56]  W. Broecker,et al.  Origin of the northern Atlantic's Heinrich events , 1992 .

[57]  André Berger,et al.  Insolation values for the climate of the last 10 , 1991 .