Carbon Isotope Measurements of Surface Seawater from a Time-Series Site off Southern California
dc.contributor.author | Hinger, Elise N. | |
dc.contributor.author | Santos, Guaciara M. | |
dc.contributor.author | Druffel, Ellen R. M. | |
dc.contributor.author | Griffin, Sheila | |
dc.date.accessioned | 2021-02-11T20:59:00Z | |
dc.date.available | 2021-02-11T20:59:00Z | |
dc.date.issued | 2010-01-01 | |
dc.identifier.citation | Hinger, E. N., Santos, G. M., Druffel, E. R. M., & Griffin, S. (2010). Carbon isotope measurements of surface seawater from a time-series site off Southern California. Radiocarbon, 52(1), 69-89. | |
dc.identifier.issn | 0033-8222 | |
dc.identifier.doi | 10.1017/S0033822200045045 | |
dc.identifier.uri | http://hdl.handle.net/10150/653830 | |
dc.description.abstract | We report carbon isotope abundances of dissolved inorganic carbon (DIC) in surface seawater collected from a time-series site off the Newport Beach Pier in Orange County, California. These data represent the first time series of ∆14C data for a coastal southern California site. From a suite of samples collected daily from 16 October to 11 November 2004, ∆14C values averaged 32.1 +/- 4.4. Freshwater input from the Santa Ana River to our site caused ∆14C and 13C values to decrease. Since this initial set of measurements, a time-series site has been maintained from November 2004 to the present. Surface seawater has been collected bimonthly and analyzed for ∆14C, delta-13C, salinity, and sigma-CO2 concentrations. Water samples from the Santa Ana River were collected during the wet season. California sea mussels and barnacle shells, ranging from 4 to 6 months old, were also collected and analyzed. Results from May 2005 to January 2008 show no long-term changes in delta-13C DIC values. ∆14C DIC values over the 2005-2006 period averaged 33.7; high ∆14C values were observed sporadically (every 6-7 months), suggesting the presence of open water eddies at our site. Finally, in 2007, a stronger upwelling signal was apparent as indicated by correlations between ∆14C, salinity, and the Bakun index, suggesting that the ∆14C record is an indicator of upwelling in the Southern California Bight. | |
dc.language.iso | en | |
dc.publisher | Department of Geosciences, The University of Arizona | |
dc.relation.url | http://radiocarbon.webhost.uits.arizona.edu/ | |
dc.rights | Copyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved. | |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | |
dc.title | Carbon Isotope Measurements of Surface Seawater from a Time-Series Site off Southern California | |
dc.type | Article | |
dc.type | text | |
dc.identifier.journal | Radiocarbon | |
dc.description.collectioninformation | The Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information. | |
dc.eprint.version | Final published version | |
dc.description.admin-note | Migrated from OJS platform February 2021 | |
dc.source.volume | 52 | |
dc.source.issue | 1 | |
dc.source.beginpage | 69 | |
dc.source.endpage | 89 | |
refterms.dateFOA | 2021-02-11T20:59:00Z |