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Items: 6

1.

Tectonically-triggered sediment and carbon export to the Hadal zone.

Bao R, Strasser M, McNichol AP, Haghipour N, McIntyre C, Wefer G, Eglinton TI.

Nat Commun. 2018 Jan 9;9(1):121. doi: 10.1038/s41467-017-02504-1.

2.

Equatorial Pacific forcing of western Amazonian precipitation during Heinrich Stadial 1.

Zhang Y, Zhang X, Chiessi CM, Mulitza S, Zhang X, Lohmann G, Prange M, Behling H, Zabel M, Govin A, Sawakuchi AO, Cruz FW, Wefer G.

Sci Rep. 2016 Oct 25;6:35866. doi: 10.1038/srep35866.

3.

Asynchronous terrestrial and marine signals of climate change during Heinrich events.

Jennerjahn TC, Ittekkot V, Arz HW, Behling H, Pätzold J, Wefer G.

Science. 2004 Dec 24;306(5705):2236-9. Epub 2004 Dec 2.

4.

Upwelling intensification as part of the Pliocene-Pleistocene climate transition.

Marlow JR, Lange CB, Wefer G, Rosell-Mele A.

Science. 2000 Dec 22;290(5500):2288-91.

5.

Calcium carbonate hexahydrate from organic-rich sediments of the antarctic shelf: precursors of glendonites.

Suess E, Balzer W, Hesse KF, Müller PJ, Ungerer CA, Wefer G.

Science. 1982 Jun 4;216(4550):1128-31.

PMID:
17808501
6.

Stable isotopes in benthic foraminifera: seasonal variation in large tropical species.

Wefer G, Berger WH.

Science. 1980 Aug 15;209(4458):803-5.

PMID:
17753308

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