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- W2000305655 abstract "The CO2 content of the past atmosphere is a key parameter for any palaeoclimatic modelling. This parameter can be modelled from the 813C record of marine carbonates (Berner, 1991, 1994). Such models were originally constructed as sensitivity tests for a variety of input scenarios for various forcing factors, such as variations in land area, runoff, degassing rates etc. (Berner, 1991). However, the sensitivity to ~13C input was tested only by assuming a constant signal of 1%o throughout the entire Phanerozoic, which resulted in a huge feedback on the modelled CO2 content, particularly for the early Carboniferous atmosphere, (Fig. 15 in Berner, 1991). The aim of this study is to utilize two different Carboniferous ~13C records, from Europe and North America, and to test their impact on the sensitivity of CO2 modelling. The Carboniferous is a particular interesting period of Earth history, because it represents the transition from greenhouse to icehouse." @default.
- W2000305655 created "2016-06-24" @default.
- W2000305655 creator A5077101836 @default.
- W2000305655 date "1998-01-01" @default.
- W2000305655 modified "2023-09-23" @default.
- W2000305655 title "The CO2 Content of the Carboniferous Atmosphere Derived from High Resolution δ13C Records of Brachiopod Calcite — Implications for the Transition from Greenhouse to Icehouse" @default.
- W2000305655 doi "https://doi.org/10.1180/minmag.1998.62a.1.128" @default.
- W2000305655 hasPublicationYear "1998" @default.
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