Biological overprint of the geological carbon cycle

By M. Katz, J. Wright, K. Miller, B. S. Cramer, Katja Fennel, Paul G. Falkowski. 2005

196 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography, Paleontology

View Paper: https://www.semanticscholar.org/paper/e95e3af13f8d365e2431996bda7c5c3bb2ab75b8

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Michael Schulz
2. Stefan Rahmstorf
3. Manfred Mudelsee

In Oceanography

1. E. Virginia Armbrust

In Paleontology

1. E. Virginia Armbrust

Citations in the corpus

• Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion (2007, background): “…implies carbon reservoir changes linked to eccentricity forcing, possibly mediated through enhanced biological productivity and increased organic carbon burial in continental margin sediments (Woodruff and Savin, 1991; Flower and Kennett, 1993, 1994; Shevenell and Kennett, 2004; Katz et al., 2005).”
• The life of diatoms in the world's oceans (2009, background): “This initiated an era of declining atmospheric CO 2 concentrations and increasing atmospheric O 2 concentration”
• Cenozoic carbon cycle imbalances and a variable weathering feedback (2016, unknown): “The degree of coupling between Fsilw and pCO2 (i.e., strength of the feedback) can only be evaluated given knowledge of Fsilw; therefore, we use records of bulk carbonate (Katz et al., 2005; Kump, 1991) and organic (Falkowski et al., 2005) carbon isotopes (Fig.”