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Sheila Griffin

Researcher at University of California, Irvine

Publications -  67
Citations -  2808

Sheila Griffin is an academic researcher from University of California, Irvine. The author has contributed to research in topics: Dissolved organic carbon & Deep sea. The author has an hindex of 27, co-authored 67 publications receiving 2591 citations. Previous affiliations of Sheila Griffin include University of California & Society of American Military Engineers.

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Ultra small-mass AMS 14C sample preparation and analyses at KCCAMS/UCI Facility

TL;DR: In this paper, the authors developed techniques for accurately and precisely measuring samples containing less than a few hundred micrograms of carbon, using a compact AMS system (NEC 0.5 MV 1.5SDH-1).
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Magnesium perchlorate as an alternative water trap in AMS graphite sample preparation: A report on sample preparation at kccams at the University of California, Irvine

TL;DR: In this article, the authors present a brief discussion of sample preparation procedures at the Keck Carbon Cycle Accelerator Mass Spectrometer (KCCAMS), University of California, Irvine, and a systematic investigation of the use of Mg(ClO (sub 4 ) (sub 2) as an absorptive water trap, replacing the standard dry ice/ethanol cold finger in graphite sample preparation.
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Large variations of surface ocean radiocarbon: Evidence of circulation changes in the southwestern Pacific

TL;DR: Stuiver et al. as mentioned in this paper used radiocarbon (Δ14C) and stable isotope (δ18O and δ13C) records from a 323-year banded coral series collected from the southern Great Barrier Reef, Australia.
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The Keck Carbon Cycle AMS Laboratory, University of California, Irvine; initial operation and a background surprise.

TL;DR: A new radiocarbon accelerator mass spectrometry (AMS) laboratory for carbon cycle studies has been established at the University of California, Irvine as mentioned in this paper, where the 0.5MV AMS system was installed in mid-2002 and has operated routinely since October of that year.
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The radiocarbon signature of microorganisms in the mesopelagic ocean.

TL;DR: An isotopic portrait of carbon assimilation by the in situ, free-living microbial community, integrated over >50,000 L of seawater, implies that recent, photosynthetic carbon is not always the major carbon source supporting microbial community production in the mesopelagic realm.