- published: 14 Aug 2013
- views: 3853
Paleoclimatology (in British spelling, palaeoclimatology) is the study of changes in climate taken on the scale of the entire history of Earth. It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within things such as rocks, sediments, ice sheets, tree rings, corals, shells and microfossils. It then uses the records to determine the past states of the Earth's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, specifically the impact of climate on mass extinctions and biotic recovery.
The scientific study field of paleoclimate began to form in the early 19th century, when discoveries about glaciations and natural changes in Earth's past climate helped to understand the greenhouse effect.
Paleoclimatologists employ a wide variety of techniques to deduce ancient climates.
Mountain glaciers and the polar ice caps/ice sheets provide much data in paleoclimatology. Ice-coring projects in the ice caps of Greenland and Antarctica have yielded data going back several hundred thousand years, over 800,000 years in the case of the EPICA project.
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Oxygen Isotopes and the Paleoclimate Record
10th USSP Urbino Summer School on Paleoclimatology
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Chapter 14B Paleoclimatology Proxy Data.mp4
Cyber4Paleo Webinar 5: Paleobiology Database and the World Data Center for Paleoclimatology
Climate change and paleoclimatology: 2013/2014 in perspective
This episode continues our investigation of current climate change by exploring the climate of the past and the techniques used to do so in present day. Topics covered in this video: 0:00 - 1:24 - Defining paleoclimate - Why study paleoclimate? - Proxies and why they're used - What types of proxies are there? 1:25 - 3:02 - Tree rings as proxies - How they are used 3:03 - 7:59 - Ice cores as proxies - Isotopes (hydrogen and oxygen), bubbles - Antarctica and Vostok - How ice cores are used - Figure of ice core data 8:00 - 9:36 - Sedimentary particles (fossils and pollen) as proxies 9:37 - 12:58 - Diagnostic rock types - Coal deposits, salt or gypsum deposits, glaciers - Evidence of past glaciers - Moraine, smoothing striations, erra...
A brief explanation of oxygen isotopes, and how the oxygen isotope signal can be used to study past climates.
This short documentary (11 minutes) was produced in celebration of the 10th USSP in Urbino, Italy. The 10th summer school of the USSP consortium will focus on past climate dynamics with special emphasis on the analysis of the long-term carbon cycling and its implications in the understanding of present and future climates. USSP 2013 will integrate lectures, symposia, fieldtrips, and exercises on the many different areas of paleoclimatology including biogeochemical cycling, paleoceanography, continental systems, and all aspects of deep time climate modeling. This film features many senior paleoclimate scientists and tell their story on the relevance and legacy of 10 years of USSP. Credit scene music: "Love theme from The Godfather" by Nino Rota. Courtesy of Paramount Pictures.
"Paleoclimatology" is the study of changes in climate taken on the scale of the entire history of Earth. It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within rocks, sediments, ice sheets, tree rings, corals, shells and microfossils; it then uses these records to determine the past states of the Earth's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. The scientific study field of paleoclimate begun to form in the early 19th century, when discoveries about glaciations and natural changes in Earth's climate past helped to identify the process of th...
Paleoclimatology is the study of changes in climate taken on the scale of the entire history of Earth. It uses a variety of proxy methods from the Earth and life sciences to obtain data previously preserved within rocks, sediments, ice sheets, tree rings, corals, shells and microfossils; it then uses these records to determine the past states of the Earth's various climate regions and its atmospheric system. Studies of past changes in the environment and biodiversity often reflect on the current situation, and specifically the impact of climate on mass extinctions and biotic recovery. This video is targeted to blind users. Attribution: Article text available under CC-BY-SA Creative Commons image source in video
Mark D. Uhen of George Mason University talks about Paleobiology Database and David M. Anderson of NOAA's National Climatic Data Center presents on the World Data Center for Paleoclimatology.
Lynn Ingram, professor in the Department of Earth and Planetary Science at UC Berkeley