Paper No. 14
Presentation Time: 5:00 PM
POTENTIAL ENVIRONMENTAL CONSEQUENCES OF PANTHALASSAN MARGIN VOLCANISM IN THE LATE PALEOZOIC
The late Paleozoic was a time of environmental upheaval: an ice age spanning over 50 million years was terminated, and two mass extinctions ensued. These events have been correlated to increased pCO2: the collapse of the late Paleozoic ice age (LPIA) in the Early Permian corresponds to pCO2 levels of ~3500 ppmv, the end-Guadalupian extinction occurred in tandem with the eruption of the Emeishan Traps, and the end-Permian mass extinction has been attributed to the volcanism of the Siberian Traps. However, a source for increased pCO2 during the Early Permian has not been identified. It is proposed that volcanism along the >12,000 km long Panthalassan convergent margin of Gondwana amplified pCO2 levels in the Early Permian, contributing to the transition from icehouse to greenhouse conditions. Further, Panthalassan margin volcanism was continuous throughout the Permian, and this sustained input of CO2 may be the cause of decreased alpha diversity during this period. Continuous volcanism would have preemptively stressed biota so that they were less resilient during the eruptions of the Emeishan and Siberian Traps. Thus volcanism along the Panthalassan margin may have been a contributing driver to the end of the LPIA and the Middle and Late Permian mass extinctions.
Volcanism and other magmatic activity along the Panthalassan margin are recorded in volcanic and plutonic rocks in western South America, southern Africa, Antarctica, and eastern