2008•AGUFMRequires access

Carbon-13 Observations Necessitate Reduced Ocean Ventilation at the Last Glacial Maximum, but Biogeochemical Processes Explain Most of the Atmospheric Carbon Dioxide Decrease

Alessandro Giulio Tagliabue, Laurent Bopp, Didier M. Roche, Nathaëlle Bouttes, Jean‐Claude Dutay, Ramdane Alkama, Masa Kageyama, Élisabeth Michel, Didier Paillard

Open publisher page 0 citations

Abstract

This record does not include an abstract. Use the full-text link above if available.

About this research paper

What this paper is about

An abstract is not available in the OpenAlex record for this paper.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Key concepts: Biogeochemical cycle, Carbon dioxide, Carbon dioxide in Earth's atmosphere, Environmental science, Glacial period, Atmospheric sciences, Carbon cycle, Carbon fibers

Related papers

Back to paper searchBrowse research topicsOriginal source
Carbon-13 Observations Necessitate Reduced Ocean Ventilation at the Last Glacial Maximum, but Biogeochemical Processes Explain Most of the Atmospheric Carbon Dioxide Decrease — Research Paper | ScholarLens