Sources of carbon to suspended particulate organic matter in the northern Gulf of Mexico
Bibliographic Data
| ID | 19568543 |
|---|---|
| Authors | Kelsey L Rogers (0000-0002-5541-2374), Kelsey Rogers (Florida State University), Samantha Bosman (0000-0003-1697-4080, Florida State University), Samantha H Bosman, Sarah Weber (0000-0001-6774-3018), Sarah C Weber (0000-0002-0612-5598, Leibniz Institute for Baltic Sea Research Warnemünde), Cedric Magen (0000-0003-0758-2675, University of Maryland Center for Environmental Science), Joseph P Montoya (0000-0001-7197-4660, Georgia Institute of Technology), Jeffrey P Chanton (0000-0002-3303-9708, Florida State University) |
| Editors | Jody W Deming, Lisa A Miller (0000-0001-9726-3744) |
| Year | 2019 |
| Volume | 7 |
| Publication date | 2019-01-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Elementa Science of the Anthropocene (JOURNAL) |
| Journal identifiers | ISSN: 2325-1026 • E-ISSN: 2325-1026 |
| Publisher | University of California Press (PUBLISHER • US) |
| DOI | 10.1525/elementa.389 |
| OpenAlex | W2995377814 |
| Language | EN |
| Citations received | 1 |
| References cited | 46 |
Suspended particulate organic carbon (POCsusp) in the Gulf of Mexico is unique compared to other seas and oceans. In addition to surface primary production, isotopic analysis indicates that microbial cycling of oil and riverine inputs are primary sources of carbon to POCsusp in the Gulf. To characterize POCsusp from seep sites and non-seep north central Gulf (NCG) sites potentially affected by the Deepwater Horizon (DWH) spill, we analyzed 277 and 123 samples for δ13C and Δ14C signatures, respectively. Depth, partitioned into euphotic ( 300 m), was the main driver of spatial δ13C differences, with deep depths exhibiting 13C depletion. Both deep depths and proximity to sources of natural seepage resulted in 14C depletion. A two-endmember mixing model based on Δ14C indicated that sources to POCsusp were 14–29% fossil carbon at NCG sites and 19–57% at seep sites, with the balance being modern surface production. A six-component Bayesian mixing model MixSIAR, using both 13C and 14C, suggested that riverine inputs were an important carbon source to POCsusp contributing 34–46%. The influence of seeps was localized. Below the euphotic zone at seep sites, 46 ± 5% (n = 9) of the carbon in POCsusp was derived from environmentally degraded, transformed oil; away from seeps, transformed oil contributed 15 ± 4% (n = 39). We hypothesized that, at NCG sites removed from hydrocarbon seep sources, isotopic signatures would be depleted following the spill and then shift towards background-like enriched values over time. At deep depths we observed decreasing Δ14C signatures in POCsusp from 2010 to 2012, followed by isotopic enrichment from 2012 to 2014 and a subsequent recovery rate of 159‰ per year, consistent with this hypothesis and with biodegraded material from DWH hydrocarbons contributing to POCsusp
Carbon cycle · Carbon fibers · Dissolved organic carbon · Ecosystem · Isotopes of carbon · Methane · Nutrient · Organic matter · Particulates · Petroleum seep · Photic zone · Phytoplankton · Stable isotope ratio · Total organic carbon · δ13C · Atmospheric and Environmental Gas Dynamics · Chemistry · Environmental Science · Marine and coastal ecosystems · Methane Hydrates and Related Phenomena · Ecology · Environmental Chemistry · Geology · Oceanography
Scales of seafloor sediment resuspension in the northern Gulf of Mexico
Isotopic composition of sinking particles
Oil carbon entered the coastal planktonic food web during the Deepwater Horizon oil spill
Radiocarbon evidence that carbon from the Deepwater Horizon spill entered the planktonic food web of the Gulf of Mexico
Radiocarbon – A Unique Tracer of Global Carbon Cycle Dynamics
Discussion Reporting of 14 C Data
| Unique citing works | 1 |
|---|---|
| Citations per year | 0.25 |
| Citation span | 2022 - 2022 (1) |
| Citation velocity | historical |
| Highly cited | No |
| Citation types | Neutral: 1 |