Zobrazeno 1 - 10
of 349
pro vyhledávání: '"D. Martin Jones"'
Publikováno v:
The British Medical Journal, 1955 Aug . 2(4936), 440-440.
Externí odkaz:
https://www.jstor.org/stable/20332584
Publikováno v:
AAPG Bulletin. 104:1231-1259
The Niger Delta Basin is one of the most prolific hydrocarbon provinces in the world, yet the origin of the vast amounts of oil and gas found in the numerous sub-basins across the delta remains contested. A total of 180 oil samples from more than 40
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27912d174b31313c70de064f94543d89
https://doi.org/10.1306/0122201618217407
https://doi.org/10.1306/0122201618217407
Publikováno v:
British medical journal. 2(4936)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::d78257e1bb42e6b1c2426f9694933a50
https://pubmed.ncbi.nlm.nih.gov/13240143
https://pubmed.ncbi.nlm.nih.gov/13240143
Publikováno v:
Frontiers in Microbiology, Vol 5 (2014)
Availability of inorganic nutrients, particularly N and P, is often a primary control on crude oil hydrocarbon degradation in marine systems. Nevertheless, there is a paucity of information on fundamental kinetic parameters for nutrient enhanced crud
Externí odkaz:
https://doaj.org/article/a8d8b738a51b4dbfbee148e9b0de3ee3
Autor:
D. Martin Jones, Estelle Motsch, Muhammad Farhan Ul Haquee, Mike S. M. Jetten, Scott Hardy, Sabine K. Lengger, Philippe Normand, Jerome Blewett, Philippe Schaeffer, Alex Charlton, Rachel Schwartz-Narbonne, Andrew T. Crombie, Deirdre Mikkelsen, Darci Rush, Guylaine H. L. Nuijten
Bacteria play key roles in the carbon cycle. In many sediments and peatlands, methanotrophic bacteria consume a portion of released methane, reducing the emissions of this potent greenhouse gas. In marine oxygen minimum zones (OMZ) and other anoxic s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::acb03166b46b0f96b70796b11f4551f6
https://doi.org/10.5194/egusphere-egu21-8486
https://doi.org/10.5194/egusphere-egu21-8486
Autor:
Darci Rush, E. Alex Charlton, Philippe Schaeffer, Helen M. Talbot, Philippe Normand, D. Martin Jones, Rachel Schwartz-Narbonne, Jaap S. Sinninghe Damsté, Mike S. M. Jetten, Margot Schenesse, Guylaine H. L. Nuijten, Ellen C. Hopmans, Muhammad Farhan Ul Haque, J. Colin Murrell, Sabine K. Lengger
Publikováno v:
Organic Geochemistry
Organic Geochemistry, Elsevier, 2020, 143, pp.103994. ⟨10.1016/j.orggeochem.2020.103994⟩
Organic Geochemistry, 143
Organic Geochemistry, Elsevier, 2020, 143, pp.103994. ⟨10.1016/j.orggeochem.2020.103994⟩
Organic Geochemistry, 143
Anaerobic ammonium oxidation (anammox) is a significant process for bioavailable nitrogen removal from marine systems. A bacteriohopanetetrol (BHT) isomer, with unknown stereochemistry, eluting later than BHT using high performance liquid chromatogra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::021e2be9411de79d66bd487e791687c8
https://hal.archives-ouvertes.fr/hal-03378149/document
https://hal.archives-ouvertes.fr/hal-03378149/document
Autor:
Angela Sherry, O. K. Mejeha, Clare M. McCann, D. Martin Jones, Peter Leary, Ian M. Head, Neil D. Gray
Publikováno v:
Chemosphere. 237
N and P are the key limiting nutrients considered most important for the stimulation of crude oil degradation but other trace nutrients may also be important. Experimental soil microcosms were setup to investigate crude oil degradation in the context
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d69b3d37a1d1f68b6adaa92600d5237a
https://pubmed.ncbi.nlm.nih.gov/31549657
https://pubmed.ncbi.nlm.nih.gov/31549657
Akademický článek
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Publikováno v:
Clays and Clay Minerals. 58:821-836
Clay minerals are abundant in soils and sediments and often contain Fe. Some varieties, such as nontronites, contain as much as 40 wt.% Fe2O3 within their molecular structure. Several studies have shown that various Fe-reducing micro-organisms can us
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54da2de99c9e221436d875c4ffee886a
https://doi.org/10.1346/ccmn.2010.0580610
https://doi.org/10.1346/ccmn.2010.0580610