Silbert_etal_GLobal_Fish_Decline - Biomass, Size, and...

Info iconThis preview shows pages 1–3. Sign up to view the full content.

View Full Document Right Arrow Icon
DOI: 10.1126/science.1135347 , 1773 (2006); 314 Science et al. John Sibert, in the Pacific Ocean Biomass, Size, and Trophic Status of Top Predators (this information is current as of November 21, 2007 ): The following resources related to this article are available online at version of this article at: including high-resolution figures, can be found in the online Updated information and services, can be found at: Supporting Online Material found at: can be related to this article A list of selected additional articles on the Science Web sites , 3 of which can be accessed for free: cites 19 articles This article 1 article(s) on the ISI Web of Science. cited by This article has been 2 articles hosted by HighWire Press; see: cited by This article has been Ecology : subject collections This article appears in the following in whole or in part can be found at: this article permission to reproduce of this article or about obtaining reprints Information about obtaining registered trademark of AAAS. is a Science 2006 by the American Association for the Advancement of Science; all rights reserved. The title Copyright American Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005. (print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by the Science on November 21, 2007 Downloaded from
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
4. M. E. Katz, D. K. Pak, G. R. Dickens, K. G. Miller, Science 286 , 1531 (1999). 5. H. Svensen et al. , Nature 429 , 542 (2004). 6. U. Röhl, T. J. Bralower, R. D. Norris, G. Wefer, Geology 28 , 927 (2000). 7. Even this massive geological carbon-cycle perturbation is dwarfed by anthropogenic rates of carbon emissions [~0.2 gigatons (Gt) per year for PETM and 8 Gt per year for modern ( 30 )]. 8. The CCD is the depth at which the rate of calcite input from surface waters equals the rate of dissolution and, in practice, is mapped on the sea floor by the transition from carbonate-bearing (above the CCD) to carbonate- free (below the CCD) sediments. 9. J. P. Kennett, L. D. Stott, Nature 353 , 225 (1991). 10. J. C. Zachos et al. , Science 302 , 1551 (2003). 11. J. C. Zachos et al. , Science 308 , 1611 (2005). 12. A. B. Colosimo, T. J. Bralower, J. C. Zachos, Proc. ODP Sci. Res.
Background image of page 2
Image of page 3
This is the end of the preview. Sign up to access the rest of the document.

This note was uploaded on 09/28/2008 for the course EAS 1540 taught by Professor Monger during the Fall '07 term at Cornell University (Engineering School).

Page1 / 5

Silbert_etal_GLobal_Fish_Decline - Biomass, Size, and...

This preview shows document pages 1 - 3. Sign up to view the full document.

View Full Document Right Arrow Icon
Ask a homework question - tutors are online