Glaciation and erosion of Eastern Greenland at the Eocene-Oligocene transition: Insights from low-temperature thermochronology

• Main Authors: Bernard, Thomas, Steer, Philippe, Gallagher, Kerry, Szulc, Adam, Whittam, Andrew
• Other Authors: Géosciences Rennes (GR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS), Cambridge Arctic Shelf Programme (CASP), University of Cambridge UK (CAM), European Geosciences Union
• Format: Conference Object
• Language: English
• Published: HAL CCSD 2016
• Subjects: [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; [SDU.STU]Sciences of the Universe [physics]/Earth Sciences; Greenland; East Greenland
• Online Access: https://insu.hal.science/insu-01308945

International audience Climate cooling through the Late Cenozoic was important in the evolution of glaciated mountain ranges. Whilethe onset of accelerated Cenozoic exhumation is generally associated with the Quaternary at mid-latitudes, coincidentwith the local onset of glaciation, some high-latitude passive margins may have experienced earlier glaciationstarting at 30-38 Ma or even 45 Ma. To address this issue, we use a set of new AFT data from 16 sub-verticalprofiles sampled along the fjords of the central Eastern Greenland margin between 68° and 76°N, combined withnew apatite (U-Th-Sm)/He (AHe) data from selected profiles. To infer thermal histories and exhumation from theseprofiles, we use the software QTQt. The modeling results show a major phase of exhumation in the East Greenlandmargin between 68° and 76°N starting at 305 Ma. The spatial distribution of the exhumation shows that normalfaulting on East Greenland margin had no resolvable influence on exhumation related to the cooling phase. However,the timing is coincident with the dramatic worldwide fall of surface temperature at the Eocene-Oligocenetransition. We therefore suggest that a transition from an Eocene fluvial to an Oligocene glacial-dominated landscapetriggered a period of enhanced erosion. We infer from the thermal histories that around 2.71.9 km oferosion occurred close to the coast since the Eocene-Oligocene transition. This amount of erosion is consistentwith the incision of the fjords and with the effective removal of 2.31.5 km of basalt thickness, deduced by thethermal modeling of a heating phase at 555 Ma. This phase of erosion is most strongly evidenced near the coast,suggesting either that continental ice extent was limited to the coastal areas or that erosion was less efficient outsidethese areas, leading to no obvious signal in thermochronometric data further north. Overall, this study provides thefirst onshore evidence of the onset of continental ice in East Greenland margin at the Eocene-Oligocene transition(34 Ma), ...