Corpus ID: 133135245

The Campbellton Formation, New Brunswick, Canada: A Sedimentological and Paleoenvironmental Description of an Early Devonian (Emsian) Vegetated Landscape

@inproceedings{Kennedy2011TheCF,
  title={The Campbellton Formation, New Brunswick, Canada: A Sedimentological and Paleoenvironmental Description of an Early Devonian (Emsian) Vegetated Landscape},
  author={K. Kennedy},
  year={2011}
}
3.1 Strata of the Campbellton Formation, nearly 1 km thick and known for its diverse fossil assemblage of early plants, arthropods, and fish, can be divided into six facies associations, interpreted as: 1) restricted lacustrine, 2) marginal lacustrine, 3) near-shore lacustrine, 4) coastal-deltaic, 5) sandy to gravelly alluvial plain, and 6) gravelly proximal alluvial environments. Lacustrine deposits with restricted circulation, due to depth or stagnation, have fine-grained beds with well… Expand

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Lacustrine deltas in a Mesozoic alluvial sequence from Camp Hill, Antarctica
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