Zifei Yang

ORCID: 0000-0003-3350-6385
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Methane Hydrates and Related Phenomena
  • Marine and coastal ecosystems
  • Isotope Analysis in Ecology
  • Paleontology and Stratigraphy of Fossils
  • Marine Biology and Ecology Research
  • Marine and environmental studies
  • Microbial Community Ecology and Physiology
  • Marine and coastal plant biology
  • Hydrocarbon exploration and reservoir analysis
  • Cryospheric studies and observations
  • Winter Sports Injuries and Performance
  • Arctic and Antarctic ice dynamics

Cardiff University
2023-2024

Xiamen University
2019-2023

University of California, Davis
2006

California State University, Long Beach
2006

Laboratoire Méditerranéen de Préhistoire Europe Afrique
2006

Centre de Recherche et d’Enseignement de Géosciences de l’Environnement
2006

Centre National de la Recherche Scientifique
2006

Woods Hole Oceanographic Institution
2006

University of California, Santa Barbara
2006

Marine hydrocarbon seepage emits oil and gas, including methane ( approximately 30 Tg of CH(4) per year), to the ocean atmosphere. Sediments from California margin contain preserved tar, primarily formed through weathering at sea surface. We present a record variation in abundance tar sediments for past 32,000 years, providing evidence increases emissions before during Termination IA [16,000 years ago (16 ka) 14 ka] again over IB (11-10 ka). Our study provides direct increased associated...

10.1073/pnas.0601304103 article EN Proceedings of the National Academy of Sciences 2006-08-31

Despite a major effort to constrain peak sea level during the mid-Pliocene warm period, uncertainties remain large. This interval is of interest because analogous CO2 concentration present day and potential retreat large portion Antarctic Ice Sheet. The usefulness this period ice sheet model physics limited by these on level. Here we discuss efforts produce new record amplitude change from interglacial glacial periods early mid-Pliocene, which have lower than We combine with climate...

10.5194/egusphere-egu24-10892 preprint EN 2024-03-08
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