Why measure bacterial production? A reply to the comment by Jahnke and Craven

نویسندگان

  • Jonathan J. Cole Michael L. Pace
  • P. J. LEB. WILLIAMS
چکیده

dissolved organic carbon of different molecular weights from piration rates of marine plankton populations, p. 289-357. humic and clear waters. Appl. Environ. Microbial. 56: 1672In J. E. Hobbie and P. J. 1eB. Williams, [eds.], Heterotro1677. phic activity in the sea. Plenum. TURLEY, C. M., AND K. LOCHTE. 1990. Microbial response to ZWEIEL, U.L.,B. NORRMAN,AND A. HAGSTROM. 1993. Conthe input of fresh detritus to the deep-sea bed. Palaeogeogr. sumption of dissolved organic carbon by marine bacteria Palaeoclimatol. Palaeoecol. 89: 2-23. and demand for inorganic nutrients. Mar. Ecol. Prog. Ser. WILLIAMS, P. J. LEB. 1984. A review of measurements of res101: 23-32.

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تاریخ انتشار 1999