Table 1. Locality summary table.
| LATE PALEOCENE | PETM | EARLY EOCENE | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| A.1 | A.2 | B | C.1 | C.2 | D.1 | D.2 | D.3 | E.1 | E.2 | |
| Sample size (n) | 224* | 92 | 452* | 229 | 75 | 5 | 40 | 11 | 61 | 265 |
| Species richness (quarry) | 20* | 13 | 41* | 12 | 10 | 3 | 10 | 6 | 12 | 16 |
| Species richness (strat. level) | 30 | 41* | 13 | 13 | 17 | |||||
| LMAT (°C) | 18.48 ± 2.6 | 18.8* ± 2.6 | 22.3 ± 3.4 | 22.3 ± 3.9 | 19.1 ± 3.7 | |||||
| MAP (cm/year) | 145 + 62.6 −43.7 | 184* + 79.3 −55.4 | 99 + 42.7 −29.82 | 104 + 45.0 −31.4 | 142 + 61.2 −42.8 | |||||
| Lithology and depositional environment | Fluvial/lacustrine. Thinly bedded siltstone and fine-grained sandstones with plant debris and ripples | Lacustrine. Thinly bedded sand and siltstone with alternating ripple beds | Oxbow pond. Laminated bedding and fine to very fine-grained sandstone. | Fluvial. Massive sandstone body with fine-grained sediment. Big Channel complex. | Fluvial. Large sandstone body with coarse (almost gravel) to fine-grained sand. Yellow in color. | |||||
Note:
Equation (1)–(3) were used for climate reconstruction. All data collected, and analyses made by Dunn (2003) are denoted with a superscript of (*). Climate estimates for Level A were made using a pooled dataset of Dunn’s collections and the 2017 collections.