Paleoclimatology is the study of past climates. Since it is not possible to go back in time to see what climates were like, scientists use imprints created during past climate, known as proxies, to interpret paleoclimate. Microbial life, such as diatoms, forams, and coral serve as useful climate proxies. Other proxies include ice cores, tree rings, and sediment cores (which include diatoms, foraminifera, microbiota, pollen, and charcoal within the sediment and the sediment itself).
| Date Of Record Release | 2010-10-26 19:29:30 |
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| Description | Paleoclimatology is the study of past climates. Since it is not possible to go back in time to see what climates were like, scientists use imprints created during past climate, known as proxies, to interpret paleoclimate. Microbial life, such as diatoms, forams, and coral serve as useful climate proxies. Other proxies include ice cores, tree rings, and sediment cores (which include diatoms, foraminifera, microbiota, pollen, and charcoal within the sediment and the sediment itself). |
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| Source | Microbial Life |
| Keyword | Microbes |
| Selector | Selection Committee |
| Date Of Record Creation | 2010-10-26 19:16:01 |
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| Date Last Modified | 2010-10-26 19:29:30 |
| Creator | Monica Bruckner |
| Language | English |