GSA Annual Meeting in Denver, Colorado, USA - 2016

Paper No. 106-2
Presentation Time: 8:15 AM


KHOZYEM, Hassan1, ADATTE, Thierry2, MBABI BITCHONG, André2, CHEVALIER, Yoann2 and KELLER, Gerta3, (1)Department of Geology, University of Aswan, Aswan, 81528, Egypt, (2)Institute of Earth Sciences (ISTE), University of Lausanne, Lausanne, 1015, Switzerland, (3)Department of Geosciences, Princeton University, Guyot Hall, Princeton, NJ 08544,

The Paleocene-Eocene Thermal Maximum (PETM, ~55.8±0.2 Ma) is marked by a global drop of 2-6‰ in δ13C values and rapid warming of 4-5°C in tropical surface waters and 4-8°C in high latitudes. Climate warming persisted for several tens of thousands of years and resulted in rapid diversification in terrestrial mammals and marine planktic foraminifera. Deep-water bathyal benthic foraminifera suffered a mass extinction (~40% species) but no significant extinctions occurred shallow shelf environments. Benthic extinctions are commonly explained as the effects of the initial stage of climate warming due to North Atlantic Volcanic Province volcanism (NAVP), which triggered methane release from ocean sediments causing global warming and ocean acidification. But the relationship between NAPV and the PETM events are not clearly demonstrated. Several studies [1-4] demonstrated the relationship between Hg anomalies in sediments and LIP activity associated with mass extinctions. We investigated the mercury (Hg) content of several sections located in deep bathyal (Zumaya, Trabakua, N-Spain) and outer shelf environments (Dababiya GSSP, Duwi, Egypt). At Zumaya the PETM is marked by a red clayey and marly interval poor in organic matter and coincident with a pronounced δ13C negative shift. A comparable clay interval with low TOC content is also present in the Dababyia section in the lower part of the negative δ13C shift, whereas the upper part of is enriched in TOC, reflecting increased productivity. A significant but unique Hg enrichment is observed at the onset of the PETM just below the carbone isotope shift in Spain as well as in Egypt. This increase, which is not correlated with clay or total organic carbon contents, suggests the Hg anomaly resulted from higher atmospheric Hg input into the marine realm, rather than organic matter scavenging and/or increased run-off. This Hg anomaly at the onset of the PETM provides the first direct evidence that volcanism played a crucial role in triggering the PETM events by initiating the warming that likely released methane gases that accelerated greenhouse warming and ocean acidification.

 [1] Grasby et al., 2013, Geology 351, 209–216. [2] Font et al., 2016. Geology 44, 171–174. [3] Sanei et al., H., 2012, Geology 40, 63–66. [4] Percival et al., 2015, EPSL 428, 267–280. [5