Interpretation of fluvial strata in continental
basins is contingent upon recognizing stratal architectures and climate change
signals from fluvial strata, and provide insights into understanding how
fluvial sedimentation interacts with basin topography. These aspects are
difficult to assess in the pre-Devonian fluvial rock record, because
comparisons to models based on vegetated modern rivers may not be suitable. In
this paper, Lowe and Arnott carefully describe the architecture of braided and
ephemeral facies in the Cambro-Ordovician Potsdam Group in the Ottawa Embayment
and Quebec Basin in northeastern North America. The contribution reveals
pre-Devonian fluvial architectures and processes, and how they relate to global
orbitally-forced climate changes in the Late Cambrian. These aspects of
pre-Devonian fluvial sedimentology are important to the Joe Geologist because
they provide a framework to make basin-wide time-significant stratigraphic
correlations, and understand variations in stratal architectures with varying
degrees of interaction with basement topography, potentially important for
groundwater and oil migration, and discerning climate change during this
critical period.
Composition and architecture of braided and sheetflood-dominated ephemeral fluvial strata in the Cambrian–Ordovician Potsdam Group: a case example of the morphodynamics of early Phanerozoic fluvial systems and climate change by David G. Lowe and
R.W.C. Arnott
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