HelioWebGuizhou University, China
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I[Guizhou University, China]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (14)"]
CA["Linked Collaborating Authors (4)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Carbon isotope evidence for a vigorous biological pump in the wake of end-Permian mass extinction
- Constraints on Early Triassic carbon cycle dynamics from paired organic and inorganic carbon isotope records
- Patterns of Reef Ecosystem Recovery Indicate That Adverse Early Triassic Ocean Conditions Extended into Middle Triassic Time
- Prolonged and recurrent global seafloor anoxia in the Early Triassic from uranium isotopic evidence
- Ocean redox conditions during the Cryogenian interglacial period controlled by continental weathering
- DIC spatiotemporal variability and sources in permafrost catchments of the Yangtze River source region: insights from stable carbon isotope and water chemistry
- Implications of Giant Ooids for the Carbonate Chemistry of Early Triassic Oceans
- Influence of Siliciclastic Turbidites on the Evolution of a Latest Permian to Late Triassic Isolated Carbonate Platform in the Nanpanjiang Basin of South China
- Orbital forcing in the Middle Triassic of the eastern Tethys: implications for paleoclimate and eustasy
- Using Nuclear magnetic resonance sounding to characterise groundwater distribution in Yangjiashan landslide, China
- Early Triassic Weathering Intensity and Climate Recovery After the end-Permian Extinction
- Long-Term Assembly of Complex Marine Ecosystems in Tropical Reefs Following the Worst Extinction of Animal Life
- The global vulnerability of plant xylem
- Did Microbial Carbonate Flourish When Skeletal Metazoans and Algae were in Low Abundance in the Aftermath of the End-Permian Extinction?