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Items: 7

1.

Future ocean hypercapnia driven by anthropogenic amplification of the natural CO2 cycle.

McNeil BI, Sasse TP.

Nature. 2016 Jan 21;529(7586):383-6. doi: 10.1038/nature16156.

PMID:
26791726
2.

Anthropogenic changes to seawater buffer capacity combined with natural reef metabolism induce extreme future coral reef CO2 conditions.

Shaw EC, McNeil BI, Tilbrook B, Matear R, Bates ML.

Glob Chang Biol. 2013 May;19(5):1632-41. doi: 10.1111/gcb.12154. Epub 2013 Feb 26.

PMID:
23505026
3.

Southern Ocean acidification: a tipping point at 450-ppm atmospheric CO2.

McNeil BI, Matear RJ.

Proc Natl Acad Sci U S A. 2008 Dec 2;105(48):18860-4. doi: 10.1073/pnas.0806318105. Epub 2008 Nov 20.

4.

Comment on "Preindustrial to modern interdecadal variability in coral reef pH".

Matear RJ, McNeil BI.

Science. 2006 Oct 27;314(5799):595.

5.
6.

Projected climate change impact on oceanic acidification.

McNeil BI, Matear RJ.

Carbon Balance Manag. 2006 Jun 27;1:2.

7.

Anthropogenic CO2 uptake by the ocean based on the global chlorofluorocarbon data set.

McNeil BI, Matear RJ, Key RM, Bullister JL, Sarmiento JL.

Science. 2003 Jan 10;299(5604):235-9.

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