Polygonal mounds in the Barents Sea reveal sustained organic productivity towards theP-Tboundary

Author:

Alves Tiago M.1

Affiliation:

1. 3D Seismic Lab; School of Earth and Ocean Sciences; Cardiff University; Main Building, Park Place Cardiff CF10 3AT UK

Publisher

Wiley

Subject

Geology

Reference31 articles.

1. Norw. Petrol. Soc. (NPF) Spec. Publ.;Beauchamp,1993

2. Permian climatic cooling in the Canadian Arctic;Beauchamp;Geol. Soc. Am. Spec. Pap.,1994

3. Growth and demise of Permian biogenic chert along northwest Pangea: Evidence for end-Permian collapse of thermohaline circulation;Beauchamp;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2002

4. Soc. Econ. Paleontol. Mineral. Spec. Publ.;Beauchamp,1997

5. Carbonate build-up flank deposits: An example from the Permian (Barents Sea, northern Norway) challenges classical facies models;Blendinger;Sed. Geol.,1997

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