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Items: 6

1.

More efficient North Atlantic carbon pump during the Last Glacial Maximum.

Yu J, Menviel L, Jin ZD, Thornalley DJR, Foster GL, Rohling EJ, McCave IN, McManus JF, Dai Y, Ren H, He F, Zhang F, Chen PJ, Roberts AP.

Nat Commun. 2019 May 15;10(1):2170. doi: 10.1038/s41467-019-10028-z.

2.

Anomalously weak Labrador Sea convection and Atlantic overturning during the past 150 years.

Thornalley DJR, Oppo DW, Ortega P, Robson JI, Brierley CM, Davis R, Hall IR, Moffa-Sanchez P, Rose NL, Spooner PT, Yashayaev I, Keigwin LD.

Nature. 2018 Apr;556(7700):227-230. doi: 10.1038/s41586-018-0007-4. Epub 2018 Apr 11.

PMID:
29643484
3.

PALEOCEANOGRAPHY. A warm and poorly ventilated deep Arctic Mediterranean during the last glacial period.

Thornalley DJ, Bauch HA, Gebbie G, Guo W, Ziegler M, Bernasconi SM, Barker S, Skinner LC, Yu J.

Science. 2015 Aug 14;349(6249):706-10. doi: 10.1126/science.aaa9554.

4.

The deglacial evolution of North Atlantic deep convection.

Thornalley DJ, Barker S, Broecker WS, Elderfield H, McCave IN.

Science. 2011 Jan 14;331(6014):202-5. doi: 10.1126/science.1196812.

5.

Holocene oscillations in temperature and salinity of the surface subpolar North Atlantic.

Thornalley DJ, Elderfield H, McCave IN.

Nature. 2009 Feb 5;457(7230):711-4. doi: 10.1038/nature07717.

PMID:
19194447
6.

Deep flow in the Madagascar-Mascarene Basin over the last 150,000 years.

McCave IN, Kiefer T, Thornalley DJ, Elderfield H.

Philos Trans A Math Phys Eng Sci. 2005 Jan 15;363(1826):81-99.

PMID:
15598625

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