Abstract
A record of detrended mean high water (MHW) variations from Hammock River marsh, Connecticut, is extended from ca. 850 to ca. 500 cal yr A.D. and correlated with summer-temperature reconstructions from northern Fennoscandia and northern Eurasia, Greenland Ice Sheet Project 2 δ
| Original language | English |
|---|---|
| Pages (from-to) | 89-97 |
| Journal | Quaternary Research |
| Volume | 53 |
| DOIs | |
| Publication status | Published - 2001 |