Skip to main content
. 2019 Oct 15;7:e7798. doi: 10.7717/peerj.7798

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.