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Items: 7


Neodymium isotope evidence for glacial-interglacial variability of deepwater transit time in the Pacific Ocean.

Hu R, Piotrowski AM.

Nat Commun. 2018 Nov 9;9(1):4709. doi: 10.1038/s41467-018-07079-z.


Atlantic deep water provenance decoupled from atmospheric CO2 concentration during the lukewarm interglacials.

Howe JNW, Piotrowski AM.

Nat Commun. 2017 Dec 8;8(1):2003. doi: 10.1038/s41467-017-01939-w.


North Atlantic ocean circulation and abrupt climate change during the last glaciation.

Henry LG, McManus JF, Curry WB, Roberts NL, Piotrowski AM, Keigwin LD.

Science. 2016 Jul 29;353(6298):470-4. doi: 10.1126/science.aaf5529. Epub 2016 Jun 30.


North Atlantic Deep Water Production during the Last Glacial Maximum.

Howe JN, Piotrowski AM, Noble TL, Mulitza S, Chiessi CM, Bayon G.

Nat Commun. 2016 Jun 3;7:11765. doi: 10.1038/ncomms11765.


Evolution of ocean temperature and ice volume through the mid-Pleistocene climate transition.

Elderfield H, Ferretti P, Greaves M, Crowhurst S, McCave IN, Hodell D, Piotrowski AM.

Science. 2012 Aug 10;337(6095):704-9. doi: 10.1126/science.1221294.


Synchronous deglacial overturning and water mass source changes.

Roberts NL, Piotrowski AM, McManus JF, Keigwin LD.

Science. 2010 Jan 1;327(5961):75-8. doi: 10.1126/science.1178068.


Temporal relationships of carbon cycling and ocean circulation at glacial boundaries.

Piotrowski AM, Goldstein SL, Hemming SR, Fairbanks RG.

Science. 2005 Mar 25;307(5717):1933-8.

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