

UPWELLING AND RADIOCARBON RESERVOIR CORRECTION IN PERU
Abstract:
The goal of
this research is to reevaluate the reservoir effect in Peru and
calculate an improved deltaR correction than those currently used. The
new deltaR correction will be based on Protothaca asperima and Semele corrugata shells, collected
in Paracas, and Donax obesulus
collected in Puerto Salaverry and Puerto Pariñas. These shells
were collected before any nuclear weapons testing and were archived in
museums; therefore they are not affected by anthropogenic radiocarbon,
and were collected on known dates, so decay since death can be
calculated. Other species may be added if suitable specimens are found
in museums.
Each of those shells will produce at least 10 sequential samples depending on their size. The samples will be extracted through each shell’s ontogeny. Samples will weigh approximately 4mg and will be analyzed for 14C using an Accelerator Mass Spectrometer (AMS) at the University of Arizona. Each sample will be milled consecutively parallel to the shell’s growth lines from edge to umbo. Shells are thought to be between one and two years at death. Based on that age, the sample resolution varies between one and two months. Other species may produce a longer record.
These shell species will also be evaluated to assess their possible use as sea surface temperature (SST) proxies. Field work in Peru was conducted in summer 2006 and modern shells specimens were collected. Also water samples from the sites of collection were acquired. These shells will be analyzed for d18O using an isotope ratio mass spectrometer (IRMS) at high resolution through ontogeny. These measurements will be compared to instrumental SST in the areas. It is hoped that each shell will thus contain two independent proxies for both SST and upwelling.
Each of those shells will produce at least 10 sequential samples depending on their size. The samples will be extracted through each shell’s ontogeny. Samples will weigh approximately 4mg and will be analyzed for 14C using an Accelerator Mass Spectrometer (AMS) at the University of Arizona. Each sample will be milled consecutively parallel to the shell’s growth lines from edge to umbo. Shells are thought to be between one and two years at death. Based on that age, the sample resolution varies between one and two months. Other species may produce a longer record.
These shell species will also be evaluated to assess their possible use as sea surface temperature (SST) proxies. Field work in Peru was conducted in summer 2006 and modern shells specimens were collected. Also water samples from the sites of collection were acquired. These shells will be analyzed for d18O using an isotope ratio mass spectrometer (IRMS) at high resolution through ontogeny. These measurements will be compared to instrumental SST in the areas. It is hoped that each shell will thus contain two independent proxies for both SST and upwelling.

Study Area
_______________________________________________________________________

Milling procedure for shells
_______________________________________________________________________
_______________________________________________________________________

Diver Julio Bernaola, Collecting
samples at Ilo Bay
Related Publications
2006. ETAYO-CADAVID, Miguel F, ANDRUS, C. Fred T., HODGINS, Gregory W. L., and JONES, Kevin, Geosciences ONTOGENETIC RADIOCARBON VARIATION IN MODERN PRE-BOMB PERUVIAN MOLLUSK SHELLS AS A PROXY FOR UPWELLING Paper 202-1. GSA, Philadelphia Annual Meeting2006. JONES, Kevin, HODGINS, Gregory, ANDRUS, C. Fred T., and ETAYO-CADAVID, Miguel F., RADIOCARBON AND STABLE ISOTOPE VARIATION IN PRE-BOMB ARGOPECTEN SHELLS FROM PERU: IMPLICATIONS FOR CHRONOMETRY AND THE MARINE RESERVOIR CORRECTION Paper 202-2. GSA, Philadelphia Annual Meeting
Related Publications
Geological Society of America, Annual Meeting, Philadelphia, PA, October 22-25, 2006 (see abstract above)
| Lab Tour | Research
Interests |
People |
| Lab
Capabilities |
Services
and Sample
Submission |
Contact
us |
| Intro
to Mass Spectrometry |
Intro
to Stable Isotopes |
UA
Admissions |
Copyright © 2004 The University of Alabama | Disclaimer | Contact:jlambert@wgs.geo.ua.edu


