Clay mineralogy indicates a mildly warm and humid living environment for the Miocene hominoid from the Zhaotong Basin, Yunnan, ChinaDominant factors controlling glacial and interglacial variations in the treeline elevation in tropical Africa.Delayed build-up of Arctic ice sheets during 400,000-year minima in insolation variability.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China.Extra-long interglacial in Northern Hemisphere during MISs 15-13 arising from limited extent of Arctic ice sheets in glacial MIS 14Sampling strategy and climatic implication of tree-ring cellulose oxygen isotopes of Hippophae tibetana and Abies georgei on the southeastern Tibetan Plateau.Climate extremes in Loess of China coupled with the strength of deep-water formation in the North AtlanticAbrupt vegetation shifts caused by gradual climate changes in central Asia during the HoloceneDistribution of n-alkanes in Miocene loess in Qinan, western Chinese Loess Plateau, and its palaeoenvironmental implicationsInterannual to centennial variability of the South Asian summer monsoon over the past millenniumReconstruction of the vegetation distribution of different topographic units of the Chinese Loess Plateau during the HoloceneSpatial and temporal changes of prehistoric human land use in the Wei River valley, northern ChinaDanube loess stratigraphy — Towards a pan-European loess stratigraphic modelEvidence of late early Miocene aridification intensification in the Xining Basin caused by the northeastern Tibetan Plateau upliftWhere were the monsoon regions and arid zones in Asia prior to the Tibetan Plateau uplift?Correlations between microbial tetraether lipids and environmental variables in Chinese soils: Optimizing the paleo-reconstructions in semi-arid and arid regionsDistribution and vegetation reconstruction of the deserts of northern China during the mid-HoloceneEvolution of the monsoon and dry climate in East Asia during late Cenozoic: A reviewReconstructed moisture evolution of the deserts in northern China since the Last Glacial Maximum and its implications for the East Asian Summer MonsoonSpatial variations in paleowind direction during the last glacial period in north China reconstructed from variations in the anisotropy of magnetic susceptibility of loess depositsThe use of fire at Zhoukoudian: evidence from magnetic susceptibility and color measurementsTime-scale and astronomical forcing of Serbian loess–paleosol sequencesChinese deserts and sand fields in Last Glacial Maximum and Holocene OptimumMajor changes in East Asian climate in the mid-Pliocene: Triggered by the uplift of the Tibetan Plateau or global cooling?Variation of East Asian monsoon precipitation during the past 21 k.y. and potential CO2 forcingEarly Eocene Asian climate dominated by desert and steppe with limited monsoonsEvidence for northeastern Tibetan Plateau uplift between 25 and 20Ma in the sedimentary archive of the Xining Basin, Northwestern ChinaGlacial-interglacial water cycle, global monsoon and atmospheric methane changesHysteresis and thermomagnetic properties of particle-sized fractions from loess and palaeosol samples spanning 22 Myr of accumulation on the Chinese Loess PlateauMagnetostratigraphy of the Xihe loess-soil sequence and implication for late Neogene deformation of the West Qinling MountainsReconstructing prehistoric land use change from archeological data: Validation and application of a new model in Yiluo valley, northern ChinaSedimentary history of the western Bohai coastal plain since the late Pliocene: Implications on tectonic, climatic and sea-level changesAn environmental database and temporal and spatial distribution of Chinese paleoanthropological sitesThick Miocene eolian deposits on the Huajialing Mountains: The geomorphic evolution of the western Loess PlateauAn improved methodology of the modern analogues technique for palaeoclimate reconstruction in arid and semi-arid regionsCarbon isotopic compositions of pore and matrix carbonates in carbonate nodules, and origin of carbonate formationGeochemical evidence for the provenance of middle Pleistocene loess deposits in southern ChinaNeogene eolian deposits within the West Qinling Mountains: Climatic and tectonic implicationsDistribution of soil inorganic carbon storage and its changes due to agricultural land use activity in ChinaGeochemical characteristics of the Miocene eolian deposits in China: Their provenance and climate implications
P50
Q28601684-45905262-26C9-4FC7-83C6-BFDCB87E5F7FQ28757615-AA390A5F-F8EB-4919-B733-7BF93919A658Q30571946-7B6E5AA9-E2F5-4533-9403-C65441452927Q34118465-4023CB6A-B98D-4769-AA52-8BE98C0DB902Q35837895-7A7211A2-1F58-4D1C-BBDB-99126575D79DQ36368680-1C790951-A653-42D1-A438-05840EA87B06Q57146939-B724EE4E-6AD9-4665-931A-CEA0E8DAEE46Q57251460-FD9EAC60-F7A3-466A-9CBD-7772D4002A35Q57251461-CE92B1A0-3EF6-4EE0-8984-DCFCBE99D2A6Q57251463-BB03C03D-6E77-41EA-806B-73C4ADF348E4Q57251464-66474DD0-571E-4C1F-BAB8-3662A2EB8F39Q57251466-B12817AD-9725-479D-98F8-31D645FDCD2BQ57251467-50E232F1-41F7-41C2-8188-B90024A4C901Q57251468-6F13D205-BE3D-4F14-A07E-5A8F98D5BFBAQ57251469-87811ADB-EB25-4C57-8AE0-2E36866F29B2Q57251471-A56CB713-DAB5-4322-9B90-733DE0CA4233Q57251473-2FFDE1EC-2BDD-4E13-BB35-D3973599AAE6Q57251474-23D254ED-1871-4812-8C04-8FFEF5F1D7FAQ57251475-9EED9A11-EC0E-4D85-A383-8426397F20A1Q57251477-290273C6-C044-4E2F-B1A5-A86D5A0654D7Q57251480-55C9024F-6014-4621-80D5-F6269F3B758DQ57251482-99A82D2F-362E-43BA-935B-E92C3DE354C9Q57251483-EA80F148-2A90-4FC7-BF04-F4D755B45598Q57251484-45841612-2C54-4A86-B1CD-37A870F306E6Q57251487-01F283F6-F748-41BB-9623-F0E93BF5089EQ57251488-1E653172-59D5-48A6-9639-9210CAABB37EQ57251489-C73383AC-2CDC-478C-9BFA-DBCC99555B3DQ57251490-4565CBF8-87CE-4D44-B9A4-EE5DE7D6D489Q57251491-537F7208-9A67-4100-96EB-0D4FF1E2722DQ57251493-1B383851-5A26-45B8-858D-89CA7FF37D70Q57251494-BA96D855-A824-4D60-895D-D7C06464701EQ57251495-302D257E-369F-41F7-B782-D749389393FEQ57251496-CAF68E75-E44F-41F5-AE91-D096750A0D8AQ57251497-179A53A7-9051-4E57-9BA9-E4A3133780FEQ57251498-C743C197-B77D-43FC-894F-74665E37E394Q57251499-E6614881-13C4-41B6-AEE6-7C81BF98DC6AQ57251502-15A96042-1F49-4E07-B52A-F045CFDC27B3Q57251503-47D36908-04DC-4DBB-8722-4D49D87C7B9EQ57251504-F5E53147-7A8A-4586-85C4-0CE4532A11A4Q57251505-396183FF-4CED-4236-9764-19A31D9ED438
P50
description
Chinees geoloog
@nl
chinesischer Geologe
@de
chiński geolog
@pl
geolaí
@ga
geologist
@en
geologo cinese
@it
geologo txinatarra
@eu
geòleg xinès
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geólogo chino
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geólogo chinês
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name
Guo Zhengtang
@ast
Guo Zhengtang
@cy
Guo Zhengtang
@de
Guo Zhengtang
@en
Guo Zhengtang
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Guo Zhengtang
@fr
Guo Zhengtang
@ga
Guo Zhengtang
@nl
郭正堂
@zh
type
label
Guo Zhengtang
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Guo Zhengtang
@cy
Guo Zhengtang
@de
Guo Zhengtang
@en
Guo Zhengtang
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Guo Zhengtang
@fr
Guo Zhengtang
@ga
Guo Zhengtang
@nl
郭正堂
@zh
altLabel
Zhengtang Guo
@en
prefLabel
Guo Zhengtang
@ast
Guo Zhengtang
@cy
Guo Zhengtang
@de
Guo Zhengtang
@en
Guo Zhengtang
@es
Guo Zhengtang
@fr
Guo Zhengtang
@ga
Guo Zhengtang
@nl
郭正堂
@zh
P1006
P214
P244
P1006
P1053
B-6854-2008
P106
P1153
7404657546
P19
P21
P213
0000 0003 9618 9532
P214
P244
nr94014576
P31
P3829
P496
0000-0003-2259-9715
P5142
P569
1964-04-08T00:00:00Z
P734
P7859
lccn-nr94014576