Andre et al, (2006) Understanding the Paleocene Eocene Thermal Maximum, a reconstruction
Keywords Paleocene Eocene Thermal Maximum clathrate Pangea PETM
Abstract
The Paleocene Eocene Thermal Maximum is characterized by enigmatic proxy evidence suggesting warm climates, and, as inferred by numerous publications, massive marine methane hydrate (clathrate) destabilization events. The recent discovery of a near-tropical Arctic ocean however requires a review of existing hypotheses, including greenhouse forcing, to check for the trigger and the cause of events of the PETM.
Here we propose that alternately the same proxy evidence, in toto, could have been caused by another mechanism. After the breakup of the Pangaea supercontinent some 200 million years ago, North America moved in a semicircle clockwise towards the north, hinging around the Greenland - Svalbard area until Alaska and Beringia made contact. Thus the Arctic Sea became isolated and no longer had contact with open oceans. Then the evaporation of the Arctic inner sea exceeded accumulation for a prolonged period causing a significant sea level lowering in comparison with the rest of the oceans. Furthermore, the tectonic movements of the plates may have enlarged the Arctic basin as North America continued to move progressively to the southwest, lowering sea level iin the Arctic basin further.
At the start of the Eocene, 55 Ma ago, the Turgai Strait, splitting Siberia from North to South may have connected the virtually empty Arctic basin and the near-tropical Tethys sea, resulting in an Arctic basin which would have started to fill rapidly with the warm surface water of the Tethys sea, not only transporting alien biota towards the Arctic but also warming up the area. The resulting abrupt sea level drop of some 15-30 meters in a very short time would have caused a secular destabilization of the marine methane hydrates, which would then explain the remaining proxy evidence pertaining to isotope excursions and the Elmo. Hence the empty-Arctic-basin-hypothesis appears to be backed by the evidence, challenging the case for the Palaeocene Eocene Thermal Maximum to be explained primarily as an enhanced Greenhouse forcing scenario.