Mass extinction - Globe Thesis

Keyword [Mass extinction] Result: 21 - 40 \| Page: 2 of 4
21.	Mercury Spikes Suggest Volcanic Driver Of The Ordovician-Silurian Mass Extinction In South China
22.	The Pyrite Morphology Characteristics And Its Redox Significance Across G-L Boundary Of Penglaitan GSSP Section In Guangxi Autonomous Region
23.	Zn Isotope Study On The End-guadalupian Mass Extinction In The Permian
24.	Cyclostratigraphy Research On The Late Ordovician-Early Silurian Marine Strata In Yichang,Hubei,South China
25.	Carbon Isotopic Record In Ordovician Carbonates From Tarim Basin And Its Implication For Paleo-environment
26.	Ecological Modeling Of Marine And Terrestrial Paleocommunities In South China And Xinjiang During Permian And Triassic And Marine Redox Variations
27.	Changes In Sedimentary Environment And Terrestrial Paleoecology Across The Triassic-Jurassic Transition In Eastern Sichuan Basin
28.	Changes In Marine Biogeochemical Cycles And Redox Conditions During The Devonian-Carboniferous Mass Extinction Boundary
29.	Volcanic Eruption Intensity And Time Limit During The Late Permian To Early Triassic And Its Linking With The Mass Extinction And Subsequent Recovery
30.	A Study Of Source Rock Features And Sedimentary Environmental Evolution During The Late Permian In Lower Yangtze Region,Southeastern China
31.	Mechanism And Application Of Chromium Isotopes In Carbonates As A Paleo-redox Proxy
32.	High-precision Zircon U-Pb Geochronological Studies Of The Permian Ash Beds From China And North America
33.	Palaeoenvironment Change In Shallow-marine Carbonate Platform Across The Permian-Triassic Boundary In South China And Its Possible Cause
34.	Using Digital Evolution To Explore Effects Of Mass Extinction On Community Stability And Emergence Of Coordinated Stasis
35.	End-Permian Mass Extinction Of Calcareous Algae From South China
36.	Ground-based Remote Sensing Of Dust Mass Extinction Efficiency In Africa And Asia
37.	Macroevolutionary patterns in planktonic foraminifera and the recovery of pelagic ecosystems from the Cretaceous-Paleogene mass extinction
38.	Biostratigraphy, paleoenvironment and geochemistry of the late Cenomanian Oceanic Anoxic Event 2 and the Cretaceous/Tertiary boundary
39.	The diversity, ecology, climate, and preservation of marine communities in the twenty million years following the end cretaceous mass extinction
40.	Species abundance changes during mass extinction and the inverse Signor-Lipps effect: Apparent abrupt graptolite mass extinction as an artifact of sampling
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