Zobrazeno 1 - 4
of 4
pro vyhledávání: '"MEDINAUT Shipboard Scientific Party"'
Autor:
Richard D Pancost, Ioanna Bouloubassi, Giovanni Aloisi, Jaap S Sinninghe Damsté, the Medinaut Shipboard Scientific Party
Publikováno v:
Organic Geochemistry. 32:695-707
Three novel series of non-isoprenoidal dialkyl glycerol diethers with an inferred sn-1,2 stereochemistry were tentatively identified in carbonate crusts precipitated from methane-rich bottom-waters and pore-waters associated with Mediterranean mud vo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::789bc366542cf9041be3db720fe09f1c
https://doi.org/10.1016/s0146-6380(01)00015-8
https://doi.org/10.1016/s0146-6380(01)00015-8
Autor:
Sinninghe Damsté, J.S., Pancost, R.D., Bouloubassi, I., Aloisi, V., MEDINAUT Shipboard Scientific Party
Three novel series of non-isoprenoidal dialkyl glycerol diethers with an inferred sn-1,2 stereochemistry were tentatively identified in carbonate crusts precipitated from methane-rich bottom-waters and pore-waters associated with Mediterranean mud vo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::90038126a7e4a710f038aa7cd14ab22c
https://dspace.library.uu.nl/handle/1874/4490
https://dspace.library.uu.nl/handle/1874/4490
Autor:
Pancost, Richard D., Bouloubassi, Ioanna, Aloisi, Giovanni, Sinninghe Damsté, Jaap S., Medinaut Shipboard Scientific Party, The
Publikováno v:
Organic Geochemistry
Organic Geochemistry, 2001, 32, pp.695-707. ⟨10.1016/S0146-6380(01)00015-8⟩
Organic Geochemistry, Elsevier, 2001, 32, pp.695-707. ⟨10.1016/S0146-6380(01)00015-8⟩
Organic Geochemistry, 2001, 32, pp.695-707. ⟨10.1016/S0146-6380(01)00015-8⟩
Organic Geochemistry, Elsevier, 2001, 32, pp.695-707. ⟨10.1016/S0146-6380(01)00015-8⟩
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f9570f85e7a8d7655bf9cc930d038e52
https://hal.science/hal-00170854
https://hal.science/hal-00170854
We investigated the distributions and 13C values of biomarkers for Archaea associated with anaerobic methane oxidation in disparate settings throughout two Eastern Mediterranean mud dome fields. All major classes of archaeal lipids are present in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______101::bb92a18a9a2928b4f518fee558ef87c2
https://dspace.library.uu.nl/handle/1874/4224
https://dspace.library.uu.nl/handle/1874/4224