TY - JOUR

T1 - Late Ordovician carbonate mounds from North Greenland

T2 - a peri-Laurentian dimension to the Boda Event?

AU - Harper, David Alexander Taylor

AU - Jin, Jisuo

AU - Rasmussen, Christian Mac Ørum

PY - 2014

Y1 - 2014

N2 - Late Katian (Late Ordovician) carbonate mudmounds in the Turesø Formation, Peary Land, North Greenland, succeed normal marine faunas dominated by brachiopods, bryozoans, cephalopod and gastropod molluscs, aulaceratid stromatoporoids, corals and receptaculitid algae, in the Børglum River Formation, and are themselves succeeded by organic-rich, largely barren limestones. This peri-Laurentian succession suggests deteriorating environmental conditions from a normal marine to a more restricted basin during the Late Katian and Hirnantian, against a background of gradual marine regression following the peak of the Boda Warming Event. The generally low-energy depositional setting probably lay within the Inter-Tropical Convergence Zone on the equator.

AB - Late Katian (Late Ordovician) carbonate mudmounds in the Turesø Formation, Peary Land, North Greenland, succeed normal marine faunas dominated by brachiopods, bryozoans, cephalopod and gastropod molluscs, aulaceratid stromatoporoids, corals and receptaculitid algae, in the Børglum River Formation, and are themselves succeeded by organic-rich, largely barren limestones. This peri-Laurentian succession suggests deteriorating environmental conditions from a normal marine to a more restricted basin during the Late Katian and Hirnantian, against a background of gradual marine regression following the peak of the Boda Warming Event. The generally low-energy depositional setting probably lay within the Inter-Tropical Convergence Zone on the equator.

KW - carbonate mounds

KW - Greenland

KW - Katian

KW - Late Ordovician

KW - Peary Land

U2 - 10.1080/11035897.2013.865669

DO - 10.1080/11035897.2013.865669

M3 - Journal article

AN - SCOPUS:84901245968

VL - 136

SP - 95

EP - 99

JO - G F F

JF - G F F

SN - 1103-5897

IS - 1

ER -