Dangpeng Xi
China University of Geosciences, Beijing
Activity
2024
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WHAT CAUSED THE MAJOR BIOTIC TURNOVER IN SHALLOW MARINE SETTINGS DURING THE PETM EVENT: CHANGE IN THE SEA-LEVEL OR SEA SURFACE TEMPERATURES? (INSIGHTS FROM EASTERN NEO-TETHYS)
77 D9. Recent Advances in Paleoclimatology/PaleoceanographyMonday, 23 September 20248:00 AM - 12:00 PM207D
2018
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THE DIVERSITY PATTERN OF LARGER BENTHIC FORAMINIFERA DURING THE MIDDLE EOCENE CLIMATIC OPTIMUM IN THE NORTHERN INDIAN PLATE MARGIN (PAKISTAN, EASTERN TETHYS)
T212 Cushman Foundation Symposium: Hothouse to Coldhouse Transitions at Southern High Paleolatitudes during the Cretaceous and CenozoicTuesday, 6 November 20181:30 PM - 5:30 PMRoom 140
2016
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PALYNOLOGICAL INSIGHT INTO THE K–PG BOUNDARY IN THE SONGLIAO BASIN, NE CHINA
344 Stratigraphy (Posters)Wednesday, 28 September 20169:00 AM - 6:30 PMExhibit Hall E/F
2015
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CRETACEOUS TERRESTRIAL BIOTA AND LAKE ENVIRONMENT IN NE CHINA
3 Paleontology: Ancient Life in Deep Time: Temporal and Geographic Trends in Fossil DistributionsSunday, 1 November 20158:00 AM - 12:00 PMRoom 316
2010
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CRETACEOUS LACUSTRINE ENVIRONMENTAL CHANGE OF THE SONGLIAO BASIN, NE CHINA: CASE STUDY OF SK-1 COREHOLE
231 Rapid Environmental/Climate Change in the Cretaceous Greenhouse WorldWednesday, 3 November 20108:00 AM - 12:00 PMRoom 502