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Items: 5

1.

Fueled by methane: deep-sea sponges from asphalt seeps gain their nutrition from methane-oxidizing symbionts.

Rubin-Blum M, Antony CP, Sayavedra L, Martínez-Pérez C, Birgel D, Peckmann J, Wu YC, Cardenas P, MacDonald I, Marcon Y, Sahling H, Hentschel U, Dubilier N.

ISME J. 2019 Jan 15. doi: 10.1038/s41396-019-0346-7. [Epub ahead of print]

PMID:
30647460
2.
3.

Short-chain alkanes fuel mussel and sponge Cycloclasticus symbionts from deep-sea gas and oil seeps.

Rubin-Blum M, Antony CP, Borowski C, Sayavedra L, Pape T, Sahling H, Bohrmann G, Kleiner M, Redmond MC, Valentine DL, Dubilier N.

Nat Microbiol. 2017 Jun 19;2:17093. doi: 10.1038/nmicrobiol.2017.93.

4.

First evidence for the presence of iron oxidizing zetaproteobacteria at the Levantine continental margins.

Rubin-Blum M, Antler G, Tsadok R, Shemesh E, Austin JA Jr, Coleman DF, Goodman-Tchernov BN, Ben-Avraham Z, Tchernov D.

PLoS One. 2014 Mar 10;9(3):e91456. doi: 10.1371/journal.pone.0091456. eCollection 2014.

5.

Hydrocarbon-related microbial processes in the deep sediments of the Eastern Mediterranean Levantine Basin.

Rubin-Blum M, Antler G, Turchyn AV, Tsadok R, Goodman-Tchernov BN, Shemesh E, Austin JA Jr, Coleman DF, Makovsky Y, Sivan O, Tchernov D.

FEMS Microbiol Ecol. 2014 Mar;87(3):780-96. doi: 10.1111/1574-6941.12264. Epub 2013 Dec 20.

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