# Diets and environments of late pleistocene pygmy and Columbian mammoths: Isotopic evidence from Southern California

## TL;DR

This study uses isotopic analysis to compare the diets and environments of pygmy and Columbian mammoths in Late Pleistocene Southern California.

## Contribution

The study provides new isotopic evidence on the diets and paleoenvironments of coexisting mammoth species on the mainland and islands.

## Key findings

- Mammoths primarily consumed C3 vegetation, though some ate C4 or CAM plants.
- Mainland mammoths had higher δ13C values, suggesting different dietary or environmental conditions.
- Island mammoths had δ18O values similar to modern precipitation, while mainland values suggest wetter or cooler conditions.

## Abstract

Pygmy mammoths (Mammuthus exilis) and Columbian mammoths (Mammuthus columbi) coexisted on the island of Santarosae (now the Northern Channel Islands of California) until the Late Pleistocene megafaunal extinctions, but the ecology of these mammoths is not yet well explored. In this study, we reconstructed the diets and environments of Late Pleistocene pygmy and Columbian mammoths using stable isotopes in tooth enamel samples from the Northern Channel Islands and Rancho La Brea. The enamel δ13C values indicate that these mammoths primarily consumed C3 vegetation. However, a few individuals consumed significant amounts of C4 plants, CAM plants, or water-stressed woody C3 plants. The mean diet-δ13C value for mainland mammoths (−24.2 ± 1.4‰) is about 2‰ higher than that of island mammoths (−26.4 ± 1.9‰), suggesting that most mainland mammoths consumed either water-stressed C3 vegetation, or some C4 and/or CAM plants. Reconstructed δ18O values of paleo-water from the mainland are generally lower than the mean δ18O values of modern precipitation in Southern California, suggesting conditions were wetter and/or cooler than today. Reconstructed δ18O values of paleo-water from the islands are more similar to modern precipitation. δ13C-based estimates of mean annual precipitation range from 159 to 1407 mm/yr on the islands and from 28 to 387 mm/yr on the mainland. However, consumption of small amounts of C4 and/or CAM plants may have resulted in an underestimation of precipitation for the mainland. Radiometric dating of additional fossils from both localities will help clarify the links between climate change and mammoth evolution and extinction in the region.