446 results on '"Xie, Shucheng"'
Search Results
2. Decoupled terrestrial temperature and hydroclimate during the Plio-Pleistocene in the East Asian monsoonal region
3. The influence of Gram-negative bacterial community on the distribution of 3-OH-FAs in soils
4. ENSO modulates soil organic carbon retention and deposition in the East China Sea
5. Evolution of continental inputs and watermass during cretaceous oceanic anoxic event 2 in the Neo-Tethyan region: Evidence from Nd-isotopes in southern Tibet
6. Tidal restriction likely has greater impact on the carbon sink of coastal wetland than climate warming and invasive plant
7. Millennial changes and cooling trends in land surface warm-season temperatures during the Holocene
8. Marine sulfate sulfur isotopic evidence for enhanced terrestrial weathering and expansion of oceanic anoxia during the Devonian-Carboniferous transition
9. Testate amoebae (Protozoa) in lakes of the Qinghai-Tibet Plateau: Biodiversity, community structures, and protozoic biosilicification in relation to environmental properties and climate warming
10. Decreased Westerly moisture transport leads to abrupt vegetation change in northern Central Asia during late MIS3: Evidence from Zeketai Loess, Ili Basin
11. The stable carbon and hydrogen isotopic composition of microbial fatty acids traces microbial metabolism in soils and peats
12. Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China
13. Contributions of the Yangtze River and Yellow River to terrestrial organic carbon deposition in the Yangtze River Estuary during the last 700 years
14. Spatiotemporal Distribution of Microbial Tetraether Lipids in a Lake and Its Inflowing River: Implications for the Identification of Flooding Events
15. Early and late phases of the Permian–Triassic mass extinction marked by different atmospheric CO2 regimes
16. Geovirology: viruses and their roles in geological history
17. Eco-engineering approaches for ocean negative carbon emission
18. Evaluation of the wider applications of the alkanol index BNA15 as temperature proxy in a broad distribution of peat deposits
19. Archaeal lipids in soils and sediments: Water impact and consequences for microbial carbon sequestration
20. A millennium ENSO-related droughts and floods occurrences documented by fossil phytoliths in core sediments of Poyang Lake, East China
21. The response of the Dajiuhu Peatland ecosystem to hydrological variations: Implications for carbon sequestration and peatlands conservation
22. Peatland degradation in Asia threatens the biodiversity of testate amoebae (Protozoa) with consequences for protozoic silicon cycling
23. Wildfire response to rapid climate change during the Permian-Triassic biotic crisis
24. Overlooked Vital Role of Persistent Algae‐Bacteria Interaction in Ocean Recalcitrant Carbon Sequestration and Its Response to Ocean Warming.
25. Pedogenic-weathering evolution and soil discrimination by sensor fusion combined with machine-learning-based spectral modeling
26. Variations in wetland hydrology drive rapid changes in the microbial community, carbon metabolic activity, and greenhouse gas fluxes
27. Precipitation in eastern China over the past millennium varied with large-scale climate patterns
28. Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic–Jurassic transition
29. Appraisal of paleoclimate indices based on bacterial 3-hydroxy fatty acids in 20 Chinese alkaline lakes
30. Massive formation of early diagenetic dolomite in the Ediacaran ocean : Constraints on the “dolomite problem”
31. Glomalin-related soil protein distributions in the wetlands of the Liaohe Delta, Northeast China : Implications for carbon sequestration and mineral weathering of coastal wetlands
32. Variations in dissolved O2 in a Chinese lake drive changes in microbial communities and impact sedimentary GDGT distributions
33. Variation of branched tetraethers with soil depth in relation to non-temperature factors: Implications for paleoclimate reconstruction
34. Global calibration of novel 3-hydroxy fatty acid based temperature and pH proxies
35. Hydrocarbon compound evidence in marine successions of South China for frequent wildfires during the Permian-Triassic transition
36. How Does Sphagnum Growing Affect Testate Amoeba Communities and Corresponding Protozoic Si Pools? Results from Field Analyses in SW China
37. The elemental enrichments at Dajiuhu Peatland in the Middle Yangtze Valley in response to changes in East Asian monsoon and human activity since 20,000 cal yr BP
38. Holocene peatland water regulation response to ~1000-year solar cycle indicated by phytoliths in central China
39. Surface soil n-alkane molecular and δD distributions along a precipitation transect in northeastern China
40. Assessing the applicability of the long-chain diol (LDI) temperature proxy in the high-temperature South China Sea
41. Land-use change effects on protozoic silicon pools in the Dajiuhu National Wetland Park, China
42. A new sea surface temperature proxy based on bacterial 3-hydroxy fatty acids
43. Distribution of pyrolytic PAHs across the Triassic-Jurassic boundary in the Sichuan Basin, southwestern China: Evidence of wildfire outside the Central Atlantic Magmatic Province
44. The Early Pliocene global expansion of C4 grasslands: A new organic carbon-isotopic dataset from the north China plain
45. Multiple environmental and ecological controls on archaeal ether lipid distributions in saline ponds
46. Distribution of microbial lipids at an acid mine drainage site in China: Insights into microbial adaptation to extremely low pH conditions
47. A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon precipitation changes in the middle Yangtze Valley
48. Rapid response of fossil tetraether lipids in lake sediments to seasonal environmental variables in a shallow lake in central China: Implications for the use of tetraether-based proxies
49. Lipid biomarkers for the reconstruction of deep-time environmental conditions
50. East Asian hydroclimate modulated by the position of the westerlies during Termination I
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