Type:

Other

Description:

This Geotimes article provides information regarding the inference of paleoclimate (global climate change) from proxy data such as ice core (oxygen isotope) records and biota found in deep sea sediments. The article discusses the history of proxy usage, the basis of current proxies, and gaps in our understanding of carbon/material cycling and climate records.

Subjects:

    Education Levels:

    • Grade 1
    • Grade 2
    • Grade 3
    • Grade 4
    • Grade 5
    • Grade 6
    • Grade 7
    • Grade 8
    • Grade 9
    • Grade 10
    • Grade 11
    • Grade 12

    Keywords:

    foram,NSDL,Biogeochemical cycling,Microbiology,Biogeochemistry,Graduate/Professional,foraminifera,Climatology,NSDL_SetSpec_1030947,Deep Marine Environment,Life Science,Higher Education,Undergraduate (Upper Division),Undergraduate (Lower Division),Stable Isotopes,global warming,carbon,Chemistry,CO2,Ecology, Forestry and Agriculture,High School,oai:nsdl.org:2200/20061121114449878T,Geoscience,methane

    Language:

    English

    Access Privileges:

    Public - Available to anyone

    License Deed:

    Creative Commons Attribution Non-Commercial Share Alike

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