Abstract The postrifted margin of Laurentia in eastern Canada had a rugged paleomorphology, with major salients and recesses formed during the long-lasting (Ediacaran to late Early Cambrian) breakup of Rodinia. After short-lived carbonate production during the Early Cambrian, the great American carbonate bank (GACB) was firmly established in the earliest Middle Cambrian as the last rift-related event (Hawke Bay event, late Early Cambrian), and was followed by mostly passive thermal subsidence of the continental crust of Laurentia. Middle to Upper Cambrian carbonates are well preserved in the Port au Port Group in western Newfoundland (St. Lawrence promontory). Scattered outcrops of upper Middle to Upper Cambrian sedimentary rocks are found in southern and eastern Quebec (Quebec reentrant), although most of the preserved Upper Cambrian facies in the reentrant consist of nearshore to fluvial clastics unconformably overlying the Grenvillian basement. The Cambrian shallow-marine carbonates are dominated by high-energy facies with significant thrombolite reefs at the platform margin. The succession consists of large-scale transgressive-regressive cycles known as Cambrian grand cycles. Some anomalies in stacking patterns are suggestive of local tectonic events that were hypothesized based on the nature (facies and age) of carbonate clasts that accumulated on the continental slope. The Cambrian–Ordovician transition occurred at a time of a major sea level lowstand that resulted in a significant unconformity in southern Quebec and Ontario. In western Newfoundland, this sea level fall is recorded in the regressive facies of the last Cambrian grand cycle but did not culminate in subaerial exposure. The duration of the depositional hiatus at the Cambrian–Ordovician transition increases toward the west from an early Skullrockian gap in the Philipsburg thrust slice in southeastern Quebec; the hiatus covered the entire Skullrockian in eastern Ontario. A major sea level rise at or near the base of the Ordovician resulted in sedimentation on an extensive peritidal, mud-dominated, low-energy carbonate platform. This platform is known as the St. George Group (western Newfoundland), the Beekmantown Group (southwestern Quebec and Ontario), the School House Hill Group (southeastern Quebec), and the Romaine Formation (Anticosti Island). The carbonate facies are characterized by large- and small-scale depositional cycles. Two third-order cycles are well documented inwestern Newfoundland. The presence of such cycles is also proposed farther south, although their precise character still has to be documented. Multiple fifth-order meter-scale peritidal-dominated cycles have been documented in the Lower Ordovician carbonates. A diachronous change in depositional style occurred along the margin of Laurentia near the base of the Middle Ordovician. Facies patterns became controlled by faulting and accumulation rates increased significantly. These changes occurred first in the late Ibexian in southeastern Quebec and in the early Whiterockian elsewhere. At most localities, this transition is also expressed in a significant subaerial unconformity that is recognized along the entire eastern (paleosouthern) margin of Laurentia. This subaerial event is interpreted as resulting from lithosphere upwarping in front of the migrating Taconic orogenic wedge. The west-directed migration of the tectonic peripheral bulge resulted in the final destruction of the GACB as sedimentation resumed in a tectonically active foreland basin.

Abstract Lower Ordovician to lower Middle Ordovician (upper Ibexian to lower Whiterockian; upper Sauk III supersequence) subtidal to peritidal carbonates of the Romaine Formation in the western Anticosti Basin record the evolution during the early Paleozoic of the low-latitude passive margin of eastern North America. A regional paleokarst unconformity, the super-Romaine unconformity corresponding to the North American Sauk-Tippecanoe megase-quence boundary developed on top of the Romaine carbonates during the early Middle Ordovician. The regional distribution of the passive-margin carbonates below the unconformity, however, suggests that significant foreland basin tectonic activity influenced the facies patterns in the uppermost Romaine Formation before the final demise of the Lower Ordovician great American carbonate bank, leading to its eventual subaerial exposure and erosion. The Romaine Formation is mostly composed of peritidal and open-shelf carbonate rocks similar to those in age-equivalent El Paso, Ellenburger, Arbuckle, Knox, Beekmantown, and St. George Groups found along thepresent southern and eastern flanks of the North American craton. Flooding of the Precambrian basement for the first time in the area allowed deposition of a deepening to shallowing carbonate succession in the late Ibexian. A narrow coastal belt of peritidal carbonates onlapped onto the basement with time, but the Romaine platform was mostly covered byopen-marine subtidal carbonate deposits. The latter, assea level receded and offlap began, gave way to peritidal deposition in the latest Ibexian. However, a succession of lower Whiterockian subtidal limestone found locally in the offlapping carbonates indicates that open subtidal conditions resumed briefly before the super-Romaine unconformity formed. This Romaine stratigraphy suggests that two large-scale, third-order, transgressive-regressive sequences are present and can be correlated basinward into the subsurface beneath the northern part of Anticosti Island. Petrographic and geochemical interpretations combined with other geologic and geophysical data provide evidence that the Lower Ordovician carbonates were hydrothermally altered at a regional scale to form porous, structurally controlled dolostone reservoirs. These structurally controlled hydrothermal dolomite reservoirs in the Romaine Formation provide a local but significant trapping mechanism for migrating hydrocarbons along the relatively unde-formed, southwesterly dipping homoclinal succession. Their signature has been recognized along several seismic lines and has served as an exploration guide in the recent round of exploration on Anticosti Island.

Abstract: A vast area of northwest Pangea, extending from the Sverdrup Basin (Canadian Arctic) to the Barents Sea (Norwegian and Russian Arctic) was affected by a significant climatic cooling in Permian time. Warm tropical-like conditions prevailed during the Asselian and Sakmarian interval, cool to cold temperate-like conditions occurred during the Artinskian to Kazanian interval, and very cold, polar-like conditions were established during latest Permian time (undetermined Kazanian-Tatarian). This climatic deterioration led to a significant shift in the composition of biogenic sedjments. Asselian and Sakmarian shallow-water carbonates comprise abundant aragonite-secreted skeletal and non-skeletal elements (ooid, cement) dominated by abundant green algae and foraminifers, associated with a great variety of microfloral and invertebrate elements (Chloroforam Assemblage). These elements combine to form hjgji- to low- energy facies including various buildups that range from small patch reefs to barrier-like structures extending for lens of kilometers. Submarine cements formed widely in both reefal and non-reefal carbonates. Evidence of meteoric-pedogenic diagenesis is pervasive in subaerially exposed carbonates. Artinskian to Kazanian shallow-water carbonates, which are poorly- lo non-cemented by submarine phases, are dominated by bryozoans, echinoderms and brachiopods (Bryonodcrm assemblage). Fusulinaceans and colonial rugose corals locally occur in Artinskian strata (Bryonoderm-extended assemblage). Small patch reefs and larger reef-mounds are locally developed in Artinskian deposits. No reefs have been encountered in Kungurian and younger strata. There is linle evidence of meteoric-pedogenic diagenesis in subaerially exposed Artinskian carbonates and none in post-Artinskian sediments. Artinskian and younger shallow-water Bryonoderm carbonates are thoroughly cemented by clear sparry calcite of shallow and relatively early burial origin. Latest Permiaji (undetermined Kazanian-Tatarian) shallow-water sediments are dominated by spic- ulitic chert (Hyalosponge assemblage) with rrujnor lenses and patches of variably silicified Bryonoderm carbonates.