Mid-Holocene climate in Northern Minnesota
Quaternary Research
By: R. M. Forester, L.D. Delorme, and J.P. Bradbury
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Abstract
Study of Holocene ostracodes and diatoms from Elk Lake, in North-Central Minnesota, indicates that the local climate of the mid-Holocene can be subdivided into three intervals. Throughout interval 1 (ca. 7800 to 6700 yr B.P.), climate was colder and much drier than today. During intervals 2 and 3 (ca. 6700 to 4000 yr B.P.) average mean-annual air temperatures approached the modern mean (3.7??C), but warm summers persisted throughout interval 2, whereas during interval 3 warm summers fell into discrete episodes. Furthermore, average mean-annual precipitation was about 85 and 90% of modern during intervals 2 and 3, respectively. Transition times between the principal intervals were less than 50 yr. The expected effects of a retreating Laurentide Ice Sheet that initially maintained a winter-style circulation, followed by transitional climate states, and finally a near-modern circulation pattern may explain these local climatic events. ?? 1987.
Suggested Citation
Forester, R.M., Delorme, L., Bradbury, J., 1987, Mid-Holocene climate in Northern Minnesota: Quaternary Research, v. 28, no. 2, p. 263-273, https://doi.org/10.1016/0033-5894(87)90064-0.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Mid-Holocene climate in Northern Minnesota |
| Series title | Quaternary Research |
| DOI | 10.1016/0033-5894(87)90064-0 |
| Volume | 28 |
| Issue | 2 |
| Publication Date | January 20, 2017 |
| Year Published | 1987 |
| Language | English |
| Publisher | Elsevier |
| Publisher location | Amsterdam, Netheralnds |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Quaternary Research |
| First page | 263 |
| Last page | 273 |