Response to Comment on "Physical Model for the Decay and Preservation of Marine Organic Carbon"
Fast enzyme deactivation rates are not required by our physical model of organic matter decay. Instead, low effective diffusivities arising from sorption of enzymes and physical protection by minerals are sufficient. Our model predicts observed temporal trends in organic-matter decay rather than spe...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 2008-03, Vol.319 (5870), p.1616-1616 |
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| container_title | Science (American Association for the Advancement of Science) |
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| creator | Rothman, Daniel H. Forney, David C. |
| description | Fast enzyme deactivation rates are not required by our physical model of organic matter decay. Instead, low effective diffusivities arising from sorption of enzymes and physical protection by minerals are sufficient. Our model predicts observed temporal trends in organic-matter decay rather than specific rate constants. Existing statistical models of intrinsic reactivity explain observed trends empirically but not theoretically. |
| doi_str_mv | 10.1126/science.1148678 |
| format | Article |
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| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 2008-03, Vol.319 (5870), p.1616-1616 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_proquest_journals_213593590 |
| source | American Association for the Advancement of Science; Jstor Complete Legacy |
| title | Response to Comment on "Physical Model for the Decay and Preservation of Marine Organic Carbon" |
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