Author:
Dowsett Harry,Robinson Marci
Abstract
Scientists learn about Earth’s future climate by looking at geological records from the past. About 3 million years ago, most of the east coast of the United States was under water. Sediments collected on the ocean floor show that the ocean environment was warmer and supported more species back then. Some of these sediments are now exposed above water as cliffs along the James River near colonial Jamestown in southeastern Virginia. Tiny fossils and other evidence in these sediments, which we call the Yorktown Formation, show us how the environment and ecosystems were affected by global warming in the past, and they hold many clues as to what Earth may look like in the future.
Reference5 articles.
1. The Yorktown Formation: improved stratigraphy, chronology, and paleoclimate interpretations from the U.S. mid-atlantic coastal plain;Dowsett;Geosciences,2021
2. High tide of the warm pliocene: implications of global sea level for Antarctic deglaciation;Miller;Geology,2012
3. Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes;Dwyer;Philos. Transact. R. Soc. A Math. Phys. Eng. Sci.,2009
4. Isotopic temperatures from the early and mid-Pliocene of the US middle Atlantic coastal plain, and their implications for the cause of regional marine climate change;Johnson;PALAIOS,2017
5. Benthic foraminiferal and sedimentologic changes in the pliocene Yorktown Formation, Virginia, USA;Spivey;J. Foraminif. Res.,2022