Decadal Changes in the Aragonite and Calcite Saturation State of the Pacific Ocean

Richard A. Feely, Christopher L. Sabine, Robert H. Byrne, Frank J. Millero, Andrew G. Dickson, Rik Wanninkhof, Akihiko Murata, Lisa A. Miller, Dana Greeley

Research output: Contribution to journalArticlepeer-review

Abstract

Based on measurements from the WOCE/JGOFS global CO 2 survey, the CLIVAR/CO 2 Repeat Hydrography Program and the Canadian Line P survey, we have observed an average decrease of 0.34% yr −1 in the saturation state of surface seawater in the Pacific Ocean with respect to aragonite and calcite. The upward migrations of the aragonite and calcite saturation horizons, averaging about 1 to 2 m yr −1 , are the direct result of the uptake of anthropogenic CO 2 by the oceans and regional changes in circulation and biogeochemical processes. The shoaling of the saturation horizon is regionally variable, with more rapid shoaling in the South Pacific where there is a larger uptake of anthropogenic CO 2 . In some locations, particularly in the North Pacific Subtropical Gyre and in the California Current, the decadal changes in circulation can be the dominant factor in controlling the migration of the saturation horizon. If CO 2 emissions continue as projected over the rest of this century, the resulting changes in the marine carbonate system would mean that many coral reef systems in the Pacific would no longer be able to sustain a sufficiently high rate of calcification to maintain the viability of these ecosystems as a whole, and these changes perhaps could seriously impact the thousands of marine species that depend on them for survival.

Original languageAmerican English
JournalGlobal Biogeochemical Cycles
Volume26
DOIs
StatePublished - Jan 1 2012

Keywords

  • Pacific Ocean
  • acidification
  • aragonite
  • calcite
  • carbon dioxide
  • saturation state

Disciplines

  • Life Sciences

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