TY - JOUR
T1 - Intense and widespread seismicity during the end-Triassic mass extinction due to emplacement of a large igneous province
AU - Lindström, Sofie
AU - Pedersen, Gunver Krarup
AU - Schootbrugge, Bas van de
AU - Hansen, Katrine Hovedskov
AU - Kuhlmann, Natascha
AU - Thein, Jean
AU - Johansson, Leif
AU - Petersen, Henrik Ingermann
AU - Alwmark, Carl
AU - Dybkjær, Karen
AU - Weibel, Rikke
AU - Erlström, Mikael
AU - Nielsen, Lars Henrik
AU - Oschmann, Wolfgang
AU - Tegner, Christian
PY - 2015/3/19
Y1 - 2015/3/19
N2 - Multiple levels of earthquake-induced soft-sediment deformations (seismites) are concentrated in the end-Triassic mass extinction interval across Europe. The repetitive nature of the seismites rules out an origin by an extraterrestrial impact. Instead, this intense seismic activity is linked to the formation of the Central Atlantic magmatic province (CAMP). By the earliest Jurassic the seismic activity had ceased, while extrusive volcanism still continued and biotic recovery was on its way. This suggests that magmatic intrusions into sedimentary strata during early stages of CAMP formation caused emission of gases (SO2, halocarbons, polycyclic aromatic hydrocarbons) that may have played a major part in the biotic crisis.
AB - Multiple levels of earthquake-induced soft-sediment deformations (seismites) are concentrated in the end-Triassic mass extinction interval across Europe. The repetitive nature of the seismites rules out an origin by an extraterrestrial impact. Instead, this intense seismic activity is linked to the formation of the Central Atlantic magmatic province (CAMP). By the earliest Jurassic the seismic activity had ceased, while extrusive volcanism still continued and biotic recovery was on its way. This suggests that magmatic intrusions into sedimentary strata during early stages of CAMP formation caused emission of gases (SO2, halocarbons, polycyclic aromatic hydrocarbons) that may have played a major part in the biotic crisis.
U2 - 10.1130/g36444.1
DO - 10.1130/g36444.1
M3 - Journal article
SN - 0091-7613
VL - 43
SP - 387
EP - 390
JO - Geology
JF - Geology
IS - 5
ER -