CO2 Release from Pockmarks on the Chatham Rise‐Bounty Trough at the Glacial Termination

Seafloor pockmarks of varying size occur over an area of 50,000 km(2) on the Chatham Rise, Canterbury Shelf and Inner Bounty Trough, New Zealand. The pockmarks are concentrated above the flat-subducted Hikurangi Plateau. Echosounder data identify recurrent episodes of pockmark formation at similar to 100,000-year frequency coinciding with Pleistocene glacial terminations. Here we show that there are structural conduits beneath the larger pockmarks through which fluids flowed upward toward the seafloor. Large negative Delta C-14 excursions are documented in marine sediments deposited next to these subseafloor conduits and pockmarks at the last glacial termination. Modern pore waters contain no methane, and there is no negative delta C-13 excursion at the glacial termination that would be indicative of methane or mantle-derived carbon at the time the Delta C-14 excursion and pockmarks were produced. An ocean general circulation model equipped with isotope tracers is unable to simulate these large Delta C-14 excursions on the Chatham Rise by transport of hydrothermal carbon released from the East Pacific Rise as previous studies suggested. Here we attribute the Delta C-14 anomalies and pockmarks to release of C-14-dead CO2 and carbon-rich fluids from subsurface reservoirs, the most likely being dissociated Mesozoic carbonates that subducted beneath the Rise during the Late Cretaceous. Because of the large number of pockmarks and duration of the Delta C-14 anomaly, the pockmarks may collectively represent an important source of C-14-dead carbon to the ocean during glacial terminations.