Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Carl G. Johnson"'
Publikováno v:
The Military Engineer, 1947 Jan 01. 39(255), 49-49.
Externí odkaz:
https://www.jstor.org/stable/44555819
Publikováno v:
The Military Engineer, 1942 Dec 01. 34(206), 652-652.
Externí odkaz:
https://www.jstor.org/stable/44567005
Autor:
Carl G. Johnson, Valier V. Galy
Publikováno v:
Rapid Communications in Mass Spectrometry. 36
Compound-specific oxygen stable isotope analysis has been commercially available for about 20 years but the technique has been infrequently applied and practical operating knowledge is limited. Existing reactor designs and chemistry fail to fully exc
Publikováno v:
Limnology and Oceanography: Methods. 16:286-298
Autor:
Ann P. McNichol, Prosper K. Zigah, Chiara Santinelli, Li Xu, Daniel J. Repeta, David M. Karl, Carl G. Johnson
Publikováno v:
Geophysical research letters (Online) 44 (2017): 2407–2415. doi:10.1002/2016GL071348
info:cnr-pdr/source/autori:Zigah PK, McNichol AP, Xu L, Johnson C, Santinelli C, Karl D, Repeta DJ/titolo:Allochthonous sources and dynamic cycling of ocean dissolved organic carbon revealed by carbon isotopes/doi:10.1002%2F2016GL071348/rivista:Geophysical research letters (Online)/anno:2017/pagina_da:2407/pagina_a:2415/intervallo_pagine:2407–2415/volume:44
info:cnr-pdr/source/autori:Zigah PK, McNichol AP, Xu L, Johnson C, Santinelli C, Karl D, Repeta DJ/titolo:Allochthonous sources and dynamic cycling of ocean dissolved organic carbon revealed by carbon isotopes/doi:10.1002%2F2016GL071348/rivista:Geophysical research letters (Online)/anno:2017/pagina_da:2407/pagina_a:2415/intervallo_pagine:2407–2415/volume:44
We present concentration and isotopic profiles of total, size, and polarity fractionated dissolved organic carbon (DOC) from Station ALOHA (A Long-term Oligotrophic Habitat Assessment), an oligotrophic site in the North Pacific Ocean. The data show t
Autor:
Oscar A. Sosa, Lucas D. Repeta, Marianne Acker, David M. Karl, Carl G. Johnson, Edward F. DeLong, Daniel J. Repeta, Sara Ferrón
Publikováno v:
Nature Geoscience. 9:884-887
A lot of methane is emitted from oxygenated seawater, where its production should be inhibited. Seawater incubations and organic matter characterizations reveal that bacteria aerobically produce methane from phosphonates in organic matter. Biogenic m
Autor:
William D. Orsi, Marco J. L. Coolen, Jordon D. Hemingway, Cornelia Wuchter, Liviu Giosan, Mitchell Lee, Carl G. Johnson, Guillem Chust, Kuldeep D. More, Xabier Irigoien, Lijun He, Valier Galy
Publikováno v:
Scientific Reports
Scientific Reports, Vol 7, Iss 1, Pp 1-12 (2017)
Scientific Reports, Vol 7, Iss 1, Pp 1-12 (2017)
Selection of microorganisms in marine sediment is shaped by energy-yielding electron acceptors for respiration that are depleted in vertical succession. However, some taxa have been reported to reflect past depositional conditions suggesting they hav
Autor:
Daniel J. Repeta, G. Narvenkar, Rajdeep Roy, Mangesh Gauns, Carl G. Johnson, Amit Sarkar, S. W. A. Naqvi, D. M. Shenoy, T. Suresh, Siby Kurian
Publikováno v:
Biogeosciences, Vol 9, Iss 7, Pp 2485-2495 (2012)
Phytoplankton and bacterial pigment compositions were determined by high performance liquid chromatography (HPLC) and liquid chromatography-mass spectrometry (LC-MS) in two freshwater reservoirs (Tillari Dam and Selaulim Dam), which are located at th
Autor:
Arthur J. Spivack, Kai-Uwe Hinrichs, Laura R. Hmelo, John M. Hayes, Carl G. Johnson, Nils G. Holm, Sean P. Sylva, Wolfgang Bach
Publikováno v:
Proceedings of the National Academy of Sciences. 103:14684-14689
Concentrations and isotopic compositions of ethane and propane in cold, deeply buried sediments from the southeastern Pacific are best explained by microbial production of these gases in situ . Reduction of acetate to ethane provides one feasible mec
Publikováno v:
Science. 308:1007-1010
The chemical dynamics of marine dissolved organic nitrogen (DON), a reservoir featuring surface accumulations even in areas where nitrogen limits productivity, have yet to be resolved. We exploited differences in the acid lability of amide bonds with