Carbon-isotope stratigraphy across the Permian–Triassic boundary: a review
C Korte, HW Kozur - Journal of Asian Earth Sciences, 2010 - Elsevier
The Palaeozoic–Mesozoic transition is marked by distinct perturbations in the global carbon
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
The Smithian/Spathian boundary (late Early Triassic): A review of ammonoid, conodont, and carbon-isotopic criteria
The transition from the Smithian substage to the Spathian substage of the Olenekian stage
of the late Early Triassic was a critical time marked by a series of biological and …
of the late Early Triassic was a critical time marked by a series of biological and …
Mercury anomalies associated with three extinction events (Capitanian crisis, latest Permian extinction and the Smithian/Spathian extinction) in NW Pangea
Abstract Strata of Permian–Early Triassic age that include a record of three major extinction
events (Capitanian Crisis, Latest Permian Extinction and the Smithian/Spathian Extinction) …
events (Capitanian Crisis, Latest Permian Extinction and the Smithian/Spathian Extinction) …
Large vertical δ13CDIC gradients in Early Triassic seas of the South China craton: Implications for oceanographic changes related to Siberian Traps volcanism
Vertical gradients in the δ13C of seawater dissolved inorganic carbon (Δδ13CDIC) can be
estimated for paleomarine systems based on δ13Ccarb data from sections representing a …
estimated for paleomarine systems based on δ13Ccarb data from sections representing a …
Recurrent early triassic ocean anoxia
Abstract The Early Triassic record, from the Smithian stratotype, shows that the organic
carbon isotope record from northwest Pangea closely corresponds to major fluctuations in …
carbon isotope record from northwest Pangea closely corresponds to major fluctuations in …
δ13C evidence that high primary productivity delayed recovery from end-Permian mass extinction
Euxinia was widespread during and after the end-Permian mass extinction and is commonly
cited as an explanation for delayed biotic recovery during Early Triassic time. This anoxic …
cited as an explanation for delayed biotic recovery during Early Triassic time. This anoxic …
Two-stage marine anoxia and biotic response during the Permian–Triassic transition in Kashmir, northern India: pyrite framboid evidence
Although expanded ocean anoxia has long been believed to be a direct killing mechanism
causing mortality of organisms during the Permian-Triassic mass extinction, little has been …
causing mortality of organisms during the Permian-Triassic mass extinction, little has been …
Permian–Triassic boundary interval in the Middle East (Iran and N. Oman): Progressive environmental change from detailed carbonate carbon isotope marine curve …
The end Permian negative δ13C excursion is well known but its cause and chronology are
still in question. In an attempt to decipher the timing and reasons for this strong decrease, we …
still in question. In an attempt to decipher the timing and reasons for this strong decrease, we …
Global oolite deposits across the Permian–Triassic boundary: a synthesis and implications for palaeoceanography immediately after the end-Permian biocrisis
Abstract The Permian–Triassic mass extinction (PTME) is not only a dramatic loss in
biodiversity and major change in ecosystem structures, but also coincided with the formation …
biodiversity and major change in ecosystem structures, but also coincided with the formation …
Cooling-driven oceanic anoxia across the Smithian/Spathian boundary (mid-Early Triassic)
Abstract The Smithian/Spathian boundary (SSB) represents a major climatic-oceanic-biotic
event within the~ 5-Myr-long recovery interval of the Early Triassic following the end …
event within the~ 5-Myr-long recovery interval of the Early Triassic following the end …