| 词条 | Thure E. Cerling |
| 释义 |
}}{{Infobox scientist |name = Thure E. Cerling |residence = Salt Lake City, Utah, United States |nationality = United States |fields = Geology Geophysics Geochemistry Biology |known_for = Modern animal diet and physiology Geological record of ecological change |awards = Fellow, National Academy of Sciences (2001) }} Thure E. Cerling (b. 1949)[1] is a Distinguished Professor of Geology and Geophysics and a Distinguished Professor of Biology at the University of Utah.[2] Cerling is a leading expert in the evolution of modern landscapes including modern mammals and their associated grassland ecologies and stable isotope analyses of the atmosphere.[3] Cerling lives in Salt Lake City, Utah. "A single hair can determine a person's location during the past weeks or even years" – Thure E. Cerling{{Attribution needed|date=February 2011}} Cerling's research interests are primarily focused on Earth surface geochemistry processes and on the geological record of ecological change.[3] Particularly, working on conservation biology, Cerling has analyzed the modern animal diet and physiology by using stable isotopes as natural tracers as well as studying dietary changes of different mammalian lineages extending over millions of years. Emphasizing continental ecologies of lakes and modern soils and ecosystems, Cerling has written extensievely about the evolution of ecosystems, the inception and strengthening of monsoons, and the atmosphere over geological time scales through evidence gathered about the fractionation of stable istopes in these systems. Current research work includes a focus on the development of landforms in semi-arid regions, the geology of Old World paleo-anthropologic sites and on contaminant migration in surface and ground waters, including the use of tritium and helium as hydrological tracers. Early lifeThure E. Cerling received his Bachelor of Science degree in geology and chemistry from Iowa State University, in Ames, Iowa, in 1972, and, in 1973, his Master of Science in geology from Iowa State. In 1977 he was awarded a Ph.D. in geology from the University of California at Berkeley. From 1977 to 1979 he worked as a research scientist at Oak Ridge National Laboratory and, from 1979 he has been a member of the University of Utah's faculty. Global ecological changesWith the publication of "Expansion of C4 ecosystems as an indicator of global ecological change in the late Miocene" in 1993, Cerling, helped by Yang Wang and Jay Quade, made relevant studies relatively to carbon isotopes. Thanks to a deep analysis of palaeovegetation from palaeosols and palaeodiet measured in fossil tooth enamel, was demonstrated a global increase in the biomass of plants using C4 photosynthesis between 7 and 5 million years ago. The decrease of atmospheric CO2 concentrations over the history below a threshold that favored the C3-photosynthesizing plants was considered as a valid reason for the global expansion of C4 biomass. The publication "Global vegetation change through the Miocene/Pliocene boundary" in 1997 confirmed these results, demonstrating even how at lower latitudes the change appeared to occur earlier because of the threshold for C3 photosynthesis is higher at warmer temperatures. Give me a hair and I'll tell you where you have been.Thure Cerling and James Ehleringer, a biology professor at the University of Utah, founded Isoforensics in 2003, a company with the aim of interpreting the stable isotope composition of various biological and synthetic materials. This was the first step for the discovery they made which was first published on February 25, 2008, by the "Proceedings of the National Academy of Sciences" with the title "Hydrogen and oxygen isotope ratios in human hair are related to geography". To know where people have been and where they lived for a while are information that became available by analyzing the stable isotope composition of their scalp hair. Cerling discovered that a strand of hair could provide valuable clues about a person's travels by studying the variation of hydrogen-2 (δ2H) and oxygen-18 (δ18O) isotopes and comparing them to the ones in the drinking water. The extent of the information that can be deduced depends on the length of the hair: the longer is the hair, the greater is the extraction of information. The variation with geography of isotope concentrations is linked with precipitations, cloud temperatures and with the amount of water that evaporates from soil and plants. When clouds move off the ocean towards inland the ratios of oxygen-18 to oxygen-16 and hydrogen-2 to hydrogen-1 tend to decrease because of the rain water with oxygen-18 and hydrogen-2, being heavier, tends to fall first. Samples of tap water were collected from more than 600 cities across the United States as well as hair samples from the barbershops in 65 cities in 20 states. The comparison showed that both hair and drinking water samples had the same isotopic variations. In order to display these information, the scientists produced color-coded maps based on the correlation of the isotopes in hair to those in drinking water. This maps show how ratios of hydrogen and oxygen isotopes in scalp hair vary in different areas of the United States. It was so proved that the water drank by a human being leaves in the hair an evidence which contain oxygen and hydrogen isotopes equal to the ones in the tap water. This technique would have been a new tool for policemen, anthropologists, archaeologists and doctors. The elephant tail hair: how many things they can say!Professor Cerling, helped by James Ehleringer and Christopher Remien (two University of Utah colleagues), George Wittemyer of Colorado State University and member of "Save the Elephants" in Nairobi, and Iain Douglas-Hamilton, who founded the association "Save the Elephants", conducted a research around the Samburu and Buffalo Springs national reserves in northern Kenya analyzing carbon and other stable isotopes in elephant tail hair to discover where and what Victoria, Anastasia and Cleopatra, three daughters of a mother elephant named Queen Elizabeth, usually eat over a six-years period (2000–2006). In order to monitor their life, the elephants were equipped with a Global Positioning System that recorded their positions every hour for the whole research period. For getting the sample of tail hair, elephants were immobilized with drug-filled dart guns when necessary. Considering that the hair grows about an inch per month, a single hair contained isotopic information to diet during an 18-month period. Wet and dry seasons: different responsesThe analysis of ratios of carbon-13 to carbon-12 along the length of a single elephant hair led Cerling and his crew to understand the elephants' diet. During the wet season, after the grass had grown long enough for elephants to grab with their trunks, their tail hair showed the presence of different form of carbon, indicating a high amount of high-protein grass. On the other hand, during the dry season, the results obtained by the analysis of the hair pointed out how elephants had switched over to shrubs and trees. Birth and CattleFor what concern the Samburu-Buffalo Springs, five weeks after the rainy season had started, the grass became rich in nutrients and the females were most likely to conceive, giving birth 22 months later, just in time for another rainy season to provide nutrients to the grass they would have eaten: the cycle could restart. The research also pointed out how developed is the competition between elephants and cattle: during the typical wet season diet of elephants, the overgrazing by cattle caused the grass to be very short, resulting in a limited access to it for elephants, out-competing them. This situation could have influenced the elephants' ability to bulk up for pregnancy. BehaviorAll these analyses pointed out even that there are some elephant families friendlier than others and showed how there are dominant families that settle down in the best places, where there is plenty of food and water. Publications by Cerling
References1. ^{{cite web |last1=Downey |first1=Philip |title=Profile of Thure E. Cerling |url=https://www.pnas.org/content/107/35/15326 |website=Proceedings of the National Academy of Sciences |publisher=Proceedings of the National Academy of Sciences |accessdate=29 March 2019}} 2. ^{{cite journal|last=Downey|first=P.|title=Profile of Thure E. Cerling|journal=Proceedings of the National Academy of Sciences|date=August 2010|volume=107|issue=35|pages=15326–15328|doi=10.1073/pnas.1010204107|pmid=20696920|pmc=2932575}} 3. ^1 {{cite web|title=Member Citation, Thure E. Cerling|url=http://nas.nasonline.org/site/Dir/529267176?pg=vprof&mbr=1002098&returl=http%3A%2F%2Fnas.nasonline.org%2Fsite%2FDir%2F529267176%3Fpg%3Dsrch%26view%3Dbasic&retmk=search_again_link|publisher=National Academy of Sciences|accessdate=22 October 2012}} External links 10 : 1949 births|Living people|Geochemistry|Members of the United States National Academy of Sciences|Fellows of the American Association for the Advancement of Science|University of Utah faculty|ISI highly cited researchers|Iowa State University alumni|University of California, Berkeley alumni|Oak Ridge National Laboratory people |
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