{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,3]],"date-time":"2025-10-03T22:21:08Z","timestamp":1759530068471},"reference-count":5,"publisher":"American Geophysical Union (AGU)","issue":"2","license":[{"start":{"date-parts":[[2012,9,21]],"date-time":"2012-09-21T00:00:00Z","timestamp":1348185600000},"content-version":"vor","delay-in-days":9244,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Global Biogeochemical Cycles"],"published-print":{"date-parts":[[1987,6]]},"abstract":"<jats:p>Until reliable procedures have been developed to preserve the phosphorus contained in particulate matter captured by in situ pumps and sediment traps and until these procedures are applied over a wide range of locations and depths in the sea, indirect methods will have to be used to determine the C\/P ratio in marine detritus. We have taken two such approaches: (1) the use of C\/N ratios for particulates captured in the upper thermocline in conjunction with 0<jats:sub>2<\/jats:sub>\/P and N\/P ratios obtained from deconvolutions of ocean chemical data and (2) regression along isopycnals in the deep\u2010sea waters free of fossil fuel CO<jats:sub>2<\/jats:sub>. While neither approach yields a definitive answer, both suggest that a value of 127 carbon atoms per phosphorus atom would be a more appropriate interim value than that of 106 adopted long ago by A. C. Redfield and his associates.<\/jats:p>","DOI":"10.1029\/gb001i002p00155","type":"journal-article","created":{"date-parts":[[2008,4,28]],"date-time":"2008-04-28T22:24:24Z","timestamp":1209421464000},"page":"155-161","source":"Crossref","is-referenced-by-count":48,"title":["C\/P ratios in marine detritus"],"prefix":"10.1029","volume":"1","author":[{"given":"Tsung\u2010Hung","family":"Peng","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Wallace S.","family":"Broecker","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"13","published-online":{"date-parts":[[2012,9,21]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/0079-6611(86)90024-8"},{"key":"e_1_2_1_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/JC090iC04p06925"},{"key":"e_1_2_1_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/0198-0149(87)90086-0"},{"key":"e_1_2_1_5_1","first-page":"26","volume-title":"The Sea","author":"Redfield A. C.","year":"1963"},{"key":"e_1_2_1_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/JC090iC04p06907"}],"container-title":["Global Biogeochemical Cycles"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1029%2FGB001i002p00155","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/GB001i002p00155","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,9,23]],"date-time":"2023-09-23T01:13:25Z","timestamp":1695431605000},"score":1,"resource":{"primary":{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/GB001i002p00155"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[1987,6]]},"references-count":5,"journal-issue":{"issue":"2","published-print":{"date-parts":[[1987,6]]}},"alternative-id":["10.1029\/GB001i002p00155"],"URL":"https:\/\/doi.org\/10.1029\/gb001i002p00155","archive":["Portico"],"relation":{},"ISSN":["0886-6236","1944-9224"],"issn-type":[{"value":"0886-6236","type":"print"},{"value":"1944-9224","type":"electronic"}],"subject":[],"published":{"date-parts":[[1987,6]]}}}