Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 44, Issue 5, Pages 2407-2415Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2016GL071348
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Funding
- NSF Cooperative Agreement for the Operation of a National Ocean Sciences Accelerator Mass Spectrometry Facility [OCE-0753487]
- Postdoctoral Scholar Program at the Woods Hole Oceanographic Institution
- National Ocean Sciences Accelerator Mass Spectrometry Facility
- NSF-STC Center for Microbial Oceanography Research and Education (C-MORE)
- Gordon and Betty Moore Foundation [GBMF3298, GBMF3794]
- Simons Foundation [329108]
- Division Of Ocean Sciences
- Directorate For Geosciences [1239667, 1260164] Funding Source: National Science Foundation
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We present concentration and isotopic profiles of total, size, and polarity fractionated dissolved organic carbon (DOC) from Station ALOHA (A Long-term Oligotrophic Habitat Assessment), an oligotrophic site in the North Pacific Ocean. The data show that, between the surface and 3500 m, low molecular weight (LMW) hydrophilic DOC, LMW hydrophobic DOC, and high molecular weight (HMW) DOC constitute 22-33%, 45-52%, and 23-35% of DOC, respectively. LMW hydrophilic DOC is more isotopically depleted (delta C-13 of -23.9 parts per thousand to -31.5 parts per thousand and Delta C-14 of -304 parts per thousand to -795 parts per thousand; mean age of 2850 to 15000 years) than the LMW hydrophobic DOC (delta C-13 of -22 parts per thousand to -23 parts per thousand and Delta C-14 of -270 parts per thousand to -568 parts per thousand; 2470 to 6680 years) and HMW DOC (delta C-13 of similar to-21 parts per thousand and Delta C-14 of -24 parts per thousand to -294 parts per thousand; 135-2700 years). Our analyses suggest that a large fraction of DOC may be derived from allochthonous sources such as terrestrial and hydrothermal DOC and cycle on much longer time scales of > 10000 years or enter the ocean as preaged carbon.
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