12.007 Geobiology, Spring 2009
This course introduces parallel evolution of life and the environment. Life processes are influenced by chemical and physical processes in the atmosphere, hydrosphere, cryosphere and the solid earth. In turn, life can influence chemical and physical processes on our planet. This course introduces th...
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Format: | Learning Object |
Language: | en-US |
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2009
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Online Access: | http://hdl.handle.net/1721.1/86310 |
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author | Summons, Roger Bosak, Tanja |
author2 | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences |
author_facet | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Summons, Roger Bosak, Tanja |
author_sort | Summons, Roger |
collection | MIT |
description | This course introduces parallel evolution of life and the environment. Life processes are influenced by chemical and physical processes in the atmosphere, hydrosphere, cryosphere and the solid earth. In turn, life can influence chemical and physical processes on our planet. This course introduces the concept of life as a geological agent and examines the interaction between biology and the earth system during the roughly four billion years since life first appeared. |
first_indexed | 2024-09-23T15:51:49Z |
format | Learning Object |
id | mit-1721.1/86310 |
institution | Massachusetts Institute of Technology |
language | en-US |
last_indexed | 2025-03-10T13:23:25Z |
publishDate | 2009 |
record_format | dspace |
spelling | mit-1721.1/863102025-02-26T17:35:07Z 12.007 Geobiology, Spring 2009 Geobiology Summons, Roger Bosak, Tanja Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences carbon cycle isotopic analysis geobiochemistry climate climate change Snowball earth mesozoic proterozoic mass extinctions paleoclimate antiquity of life carbon dating origin of life phylogenic trees This course introduces parallel evolution of life and the environment. Life processes are influenced by chemical and physical processes in the atmosphere, hydrosphere, cryosphere and the solid earth. In turn, life can influence chemical and physical processes on our planet. This course introduces the concept of life as a geological agent and examines the interaction between biology and the earth system during the roughly four billion years since life first appeared. 2009-06 Learning Object 12.007-Spring2009 local: 12.007 local: IMSCP-MD5-ea811cc7ca4c71f59e2537aaa0018e7e http://hdl.handle.net/1721.1/86310 en-US Usage Restrictions: This site (c) Massachusetts Institute of Technology 2014. Content within individual courses is (c) by the individual authors unless otherwise noted. The Massachusetts Institute of Technology is providing this Work (as defined below) under the terms of this Creative Commons public license ("CCPL" or "license") unless otherwise noted. The Work is protected by copyright and/or other applicable law. Any use of the work other than as authorized under this license is prohibited. By exercising any of the rights to the Work provided here, You (as defined below) accept and agree to be bound by the terms of this license. The Licensor, the Massachusetts Institute of Technology, grants You the rights contained here in consideration of Your acceptance of such terms and conditions. Usage Restrictions: Attribution-NonCommercial-ShareAlike 3.0 Unported http://creativecommons.org/licenses/by-nc-sa/3.0/ text/html Spring 2009 |
spellingShingle | carbon cycle isotopic analysis geobiochemistry climate climate change Snowball earth mesozoic proterozoic mass extinctions paleoclimate antiquity of life carbon dating origin of life phylogenic trees Summons, Roger Bosak, Tanja 12.007 Geobiology, Spring 2009 |
title | 12.007 Geobiology, Spring 2009 |
title_full | 12.007 Geobiology, Spring 2009 |
title_fullStr | 12.007 Geobiology, Spring 2009 |
title_full_unstemmed | 12.007 Geobiology, Spring 2009 |
title_short | 12.007 Geobiology, Spring 2009 |
title_sort | 12 007 geobiology spring 2009 |
topic | carbon cycle isotopic analysis geobiochemistry climate climate change Snowball earth mesozoic proterozoic mass extinctions paleoclimate antiquity of life carbon dating origin of life phylogenic trees |
url | http://hdl.handle.net/1721.1/86310 |
work_keys_str_mv | AT summonsroger 12007geobiologyspring2009 AT bosaktanja 12007geobiologyspring2009 AT summonsroger geobiology AT bosaktanja geobiology |