Michael Orchard - Academia.edu (original) (raw)
Native of England, educated in Hull and Cambridge. Conodont micropaleontologist with Geological Survey of Canada in Vancouver from 1979-present
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Papers by Michael Orchard
Geological Society of America Abstracts with Programs
Bulletin of Canadian Petroleum Geology, 2018
Conodonts have proven to be excellent index fossils to study the subsurface Montney Formation giv... more Conodonts have proven to be excellent index fossils to study the subsurface Montney Formation given their small size and regular occurrence in most marine facies. Twenty uppermost Permian to Lower Triassic conodont biozones are summarized and the sequence biostratigraphic framework provides a template demonstrating the correlation potential of the Montney Formation in the Peace River Basin from west-central Alberta to east-central British Columbia. The Montney Formation, which includes three 3rd order depositional sequences that are also recognized globally, naturally subdivides into Lower (Griesbachian-Dienerian; Induan), Middle (Smithian; lower Olenekian), and Upper Montney (Spathian; upper Olenekian). The Early Triassic is 4.8 m.y. in duration, but up to 200 k.y. of the latest Permian are included within the basal Montney. The ages of biozones and sequences are interpolated, but there is still considerable uncertainty in the ages for all levels, but for the base-Induan and base-A...
Geologic Time Scale 2020, 2020
Frontiers in Earth Science, Aug 23, 2023
Polar Research, Dec 1, 2008
Conodont faunas are described from Triassic sections of Svalbard, and their occurrences are local... more Conodont faunas are described from Triassic sections of Svalbard, and their occurrences are locally correlated with established ammonoid zones. With a synthesis of previous conodont-based publications, the current work presents a taxonomically up-to-date compilation of conodont data for the Triassic of Svalbard that is used to construct a conodont-based biochronology, indexed to the current lithostratigraphic nomenclature. Twenty-eight taxa spanning the earliest Griesbachian to the earliest Carnian are presented in a range chart. The examined conodont faunas are correlated with well-established conodont zonations of the Canadian Arctic, and in turn also form the basis for regional correlations.
Geological Society of America Abstracts with Programs
Bulletin of Canadian Petroleum Geology, 2018
Conodonts have proven to be excellent index fossils to study the subsurface Montney Formation giv... more Conodonts have proven to be excellent index fossils to study the subsurface Montney Formation given their small size and regular occurrence in most marine facies. Twenty uppermost Permian to Lower Triassic conodont biozones are summarized and the sequence biostratigraphic framework provides a template demonstrating the correlation potential of the Montney Formation in the Peace River Basin from west-central Alberta to east-central British Columbia. The Montney Formation, which includes three 3rd order depositional sequences that are also recognized globally, naturally subdivides into Lower (Griesbachian-Dienerian; Induan), Middle (Smithian; lower Olenekian), and Upper Montney (Spathian; upper Olenekian). The Early Triassic is 4.8 m.y. in duration, but up to 200 k.y. of the latest Permian are included within the basal Montney. The ages of biozones and sequences are interpolated, but there is still considerable uncertainty in the ages for all levels, but for the base-Induan and base-A...
Geologic Time Scale 2020, 2020
Frontiers in Earth Science, Aug 23, 2023
Polar Research, Dec 1, 2008
Conodont faunas are described from Triassic sections of Svalbard, and their occurrences are local... more Conodont faunas are described from Triassic sections of Svalbard, and their occurrences are locally correlated with established ammonoid zones. With a synthesis of previous conodont-based publications, the current work presents a taxonomically up-to-date compilation of conodont data for the Triassic of Svalbard that is used to construct a conodont-based biochronology, indexed to the current lithostratigraphic nomenclature. Twenty-eight taxa spanning the earliest Griesbachian to the earliest Carnian are presented in a range chart. The examined conodont faunas are correlated with well-established conodont zonations of the Canadian Arctic, and in turn also form the basis for regional correlations.