The latest Permian mass extinction (LPME) coincided with major changes in the composition
of marine plankton communities, yet little is known about concurrent changes in primary …

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 …

High-resolution oxygen isotope records document the timing and magnitude of global
warming across the Permian-Triassic (P-Tr) boundary. Oxygen isotope ratios measured on …

The temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …

Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for
the Permo-Triassic Boundary mass extinction, but direct evidence for an acidification event …

Recovery from the end-Permian mass extinction is frequently described as delayed,,, with
complex ecological communities typically not found in the fossil record until the Middle …

For much of the Mesozoic record there has been an inconclusive debate on the possible
global significance of isotopic proxies for environmental change and of sequence …

A high-resolution oxygen isotope record based on 356 measurements of conodont apatite
from several low latitudinal sections in South China, USA and Iran was composed in order to …

During the latest Permian extinction about 250 Myr ago, more than 90% of marine species
went extinct, and biogeochemical cycles were disrupted globally. The cause of the …

Abstract New 87 Sr/86 Sr data based on 127 well-preserved and well-dated conodont
samples from South China were measured using a new technique (LA-MC-ICPMS) based …