Abstract
Variation in ocean pH is a dynamic process occurring naturally in the upwelling zone of the California Current Large Marine Ecosystem. The nearshore carbonate chemistry is under-characterized and the physiology of local organisms may be under constant challenge from cyclical changes in pH and carbonate ion concentration of unexpectedly high magnitude. We looked to environmental pH conditions of coastal upwelling and used those values to examine effects of low pH on 4-arm larvae of purple sea urchin Strongylocentrotus purpuratus. We deployed a pH sensor at a nearshore shallow benthic site for 3weeks during summer 2010 to assess the changes in pH in the Santa Barbara Channel, a region considered to have relatively less intense upwelling along the US Pacific Coast. Large fluctuations in pH of up to 0.67 pH units were observed over short time scales of several days. Daily pH fluctuations on a tidal pattern followed temperature fluctuations over short time scales, but not over scales greater than a day. The lowest pH values recorded (~7.70) are lower than some of those pH values predicted to occur in surface oceans at the end of the century. In the context of this dynamic pH exposure, larvae were raised at elevated pCO2 levels of 1000ppm and 1450ppm CO2 (pH 7.7 and 7.5 respectively) and measured for total larval length (from the spicule tip of the postoral arm to the spicule tip of the aboral point) along the spicules, to assess effects of low pH upwelling water on morphology. Larvae in all treatments maintained normal development and developmental schedule to day 6, and did not exhibit significant differences in larval asymmetry between treatments. At day 3 and day 6, larvae in the 1450ppm CO2 treatment were significantly smaller (p<0.001) than the control larvae by only 7-13%. The observation of smaller larvae raised under high pCO2 has an as yet undetermined physiological mechanism, but has implications for locomotion and feeding. These effects of small magnitude in these urchin larvae are indicative of a potential resilience to near-future levels of ocean acidification. Using environmental monitoring of pH to inform experimental parameters provides a means to improve our understanding of acclimatization of organisms in a dynamic ecosystem.
Original language | English |
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Pages (from-to) | 288-295 |
Number of pages | 8 |
Journal | Journal of Experimental Marine Biology and Ecology |
Volume | 400 |
Issue number | 1-2 |
DOIs | |
State | Published - Apr 30 2011 |
Externally published | Yes |
Funding
We thank Dr. Dan Reed, director of the Santa Barbara Coastal Long-term Ecological Research Site (SBC LTER) for his support of this project. In particular, we are grateful to Clint Nelson of the SBC LTER for the deployment and retrieval of the SeaFET, and for the collection of water samples. We thank Christoph Pierre and Sam Hammond for the animal collection; Anna MacPherson and Evan Hunter for the assistance with alkalinity titrations; and Brittany Peterson (Scripps Institution of Oceanography) for the technical assistance and for providing the training with SeaFET operations. During the writing of this manuscript, PCY was supported by an NSF Polar Programs Postdoctoral Fellowship ( ANT 1019340 ). This study was supported in part by: (1) NSF grant OCE (OTIC) 0844394 to TRM (in support of the SeaFET development), (2) NSF grants OCE 1040960 and ANT 0944201 to GEH, and (3) funds from the University of California in support of a multi-campus research program, Ocean Acidification: A Training and Research Consortium, ( http://oceanacidification.msi.ucsb.edu/ ) to GEH and TRM. [SS]
Funders | Funder number |
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National Science Foundation | ANT 0944201, OCE (OTIC) 0844394, OCE 1040960, ANT 1019340, 1019340 |
University of California |
Keywords
- Larval morphology
- Ocean acidification
- SeaFET sensor
- Strongylocentrotus purpuratus
- Upwelling