McIntyre, David J (1999) Campanian to Paleocene dinoflagellate assemblages from the Turtle Mountain core hole, Manitoba, western Canada. Canadian Journal of Earth Sciences, 36 (5) 769-774 doi:10.1139/e98-011
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Campanian to Paleocene dinoflagellate assemblages from the Turtle Mountain core hole, Manitoba, western Canada | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | McIntyre, David J | Author | |
| Year | 1999 (May 1) | Volume | 36 |
| Issue | 5 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e98-011Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 483237 | Long-form Identifier | mindat:1:5:483237:3 |
| GUID | 0 | ||
| Full Reference | McIntyre, David J (1999) Campanian to Paleocene dinoflagellate assemblages from the Turtle Mountain core hole, Manitoba, western Canada. Canadian Journal of Earth Sciences, 36 (5) 769-774 doi:10.1139/e98-011 | ||
| Plain Text | McIntyre, David J (1999) Campanian to Paleocene dinoflagellate assemblages from the Turtle Mountain core hole, Manitoba, western Canada. Canadian Journal of Earth Sciences, 36 (5) 769-774 doi:10.1139/e98-011 | ||
| In | (1999, May) Canadian Journal of Earth Sciences Vol. 36 (5) Canadian Science Publishing | ||
| Abstract/Notes | Dinoflagellate assemblages from the Turtle Mountain core hole provide evidence for the Paleocene age of the Turtle Mountain Formation and confirm that the Boissevain Formation and the Coulter Member of the Pierre Formation are Maastrichtian. Evidence from dinoflagellates suggests that the Odonah Member of the Pierre Formation is late Campanian. The dinoflagellate assemblages indicate that nearshore shallow marine conditions were present at times during deposition of all the formations. | ||
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