Award Abstract # 1044289
RAPID Response in Gulf of Mexico: Sediment Trap Investigations

NSF Org: OCE
Division Of Ocean Sciences
Recipient: WOODS HOLE OCEANOGRAPHIC INSTITUTION
Initial Amendment Date: July 28, 2010
Latest Amendment Date: June 24, 2013
Award Number: 1044289
Award Instrument: Standard Grant
Program Manager: Thomas Janecek
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: August 1, 2010
End Date: January 31, 2014 (Estimated)
Total Intended Award Amount: $193,944.00
Total Awarded Amount to Date: $193,944.00
Funds Obligated to Date: FY 2010 = $193,944.00
History of Investigator:
  • Chris German (Principal Investigator)
    cgerman@whoi.edu
Recipient Sponsored Research Office: Woods Hole Oceanographic Institution
266 WOODS HOLE RD
WOODS HOLE
MA  US  02543-1535
(508)289-3542
Sponsor Congressional District: 09
Primary Place of Performance: Woods Hole Oceanographic Institution
266 WOODS HOLE RD
WOODS HOLE
MA  US  02543-1535
Primary Place of Performance
Congressional District:
09
Unique Entity Identifier (UEI): GFKFBWG2TV98
Parent UEI:
NSF Program(s): Marine Geology and Geophysics,
BIOLOGICAL OCEANOGRAPHY,
OCEAN DRILLING PROGRAM
Primary Program Source: 01001011DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 5987, 7914, OTHR
Program Element Code(s): 162000, 165000, 572000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Intellectual Merit: In September 2009, two time-series sediment trap and current meter moorings were deployed in the northern Gulf of Mexico to investigate biogenic fluxes settling to the seafloor (and larval recruitment) at two well-characterized and significant sites of combined deep-water coral and chemosynthetic tube-worm colonies (Fisher et al., 2007). Each of these
traps, set just above the seabed and in water depths of 400-450m, have been collecting a new sample of settling material every two weeks since 11 September 2009 and will continue to do so until 2nd July 2010 when their last sample bottle will be rotated shut and the traps will await
recovery as part of an already-funded field program (NOAA-MMS) scheduled for November. Serendipitously, however, these two traps are located just 32 nmiles to the NE and 81 nmiles to the WSW of the recent Deepwater Horizon incident and continuing oil release from the seafloor. Continuous monitoring by NOAA has shown that at least one of these two study sites became overlain by oil discharge at the ocean surface by the end of April and that both sites are now
overlain by at least light to medium concentrations of hydrocarbons ± dispersant. What remains unestablished at this point, however, is what is happening at depth and what impacts there may be at the Gulf of Mexico seafloor and, specifically, its pristine and unique deepwater coral/
chemosynthetic tube-worm colonies. The purpose of this proposal, therefore, is two-fold. First we seek to join a rapid response research cruise to the area to deploy two additional short sediment trap and current meter moorings to ensure that we maintain continuity in the sampling that began 6 months before the incident and remains ongoing at each of the two sites that we had
previously targeted as being of most significance in terms of deepwater coral/chemosynthetic tubeworm ecosystems. If we do not achieve that, our time series will end on July 2nd. Second, and anticipating that there will be a wealth of additional studies that many other PIs will wish to pursue, we seek sufficient funds to conduct initial characterization from these samples (plus
those from our earlier deployments) as soon as they are recovered (already-funded cruise in November 2010). Specifically, we anticipate generating a suite of archived samples with coregistered information on mass and biogenic flux (to include inorganic and organic carbon content) and preliminary ?finger-printing? of any hydrocarbon signatures present in each sample.
Broader Impacts: The emerging environmental impact in the Gulf of Mexico is of great societal concern and has implications for both future deepwater resource extraction and energy supply for the nation. But the majority of the attention currently being paid to the GoM system is, of necessity, focused on the shallow upper ocean where data is most readily obtained. Serendipitously, this work represents a project that can shed unique light on the effects that may
be being imparted upon remarkable and formerly pristine deepwater ecosystems in close proximity to the Deepwater Horizon well-head. Because our combined analyses will only require a small fraction of the samples we collect we will archive the remainder of each sample carefully for broader investigations and, further, we will publicize our results widely and promptly to engender such value-added research. For example, this work will clearly be of relevance and potential to other projects also being developed by (e.g.) R.Camilli (WHOI) and
C.Fisher (Penn.State). Our group stands ready to work with all such interested scientific parties and is also in contact with a film team (Mike deGruy, based in Santa Barbara) interested in a response effort (although we have no commitments to them should another team prove more suitable for that work).

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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H.K.White, P-Y.Hsing, W.Cho, T.M.Shank, E.E.Cordes, A.M.Quattrini, R.K.Nelson , R.Camilli, A.W.J.Demopoulos, C.R.German, J.M.Brooks, H.H.Roberts, W.Shedd, C.M.Reddy and C.R.Fisher. "Impact of the Deepwater Horizon oil spill on a deep-water coral community in the Gulf of Mexico" PNAS , v.109 , 2012 , p.20303-203 10.1073

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

In 2009, I began a study to collect and analyse particles sinking to the seafloor in the northern Gulf of Mexico to understand what supplied the food required to sustain delicate deep-water coral communities at depth, below sunlight, there. One obvious source is sinking of waste organic matter from the sunlit upper ocean (shallower than 200m) where life is abundant.  Alternately, nutrient supply might come from exotic chemically-fuelled ecosystems associated with natural hydrocarbon (oil and gas) seeps that are known to occur across the floor of the Gulf of Mexico, in and among the active oil fields.

While our project was already underway, the Deep Water Horizon accident occurred and within days oil slicks were mapped north of the Macondo well-head that passed directly over my sampling site.  My samples was being collected using a sediment trap which acts as a giant circular funnel with a large surface area at the top (about 3ft diameter) that narrows and empties out into a plastic bottle at its base.  Anything solid falling into the top of the funnel gets collected into the sample bottle at the base where, every two weeks, a carousel rotates to line up a fresh sample bottle with the base of the funnel (meanwhile all the other sample bottles are covered so nothing gets in or out).  That way, when we analyse the samples, we know how much material arrived at the seafloor in each 2-week period and we can analyse how things vary with time.  In this project I extended the original planned sampling so that, instead of our time-series running out while the Macondo well-head was still uncapped, we could compare, on a like-for-like basis, how the amount and composition of material sinking to the seafloor changed, from six months before the DWH accident happened until well beyond when the well-head was finally capped, several months later.

What I found, when the samples were analysed in the laboratory was that there was no immediate clear sign of oil input reaching the seafloor at the study site but that there were important results to pay attention to.  During the period that the Macondo well head was discharging oil in an uncontrolled way from the seafloor and contributing to surface ocean oil slicks, the results show an increase in the total amount of material sinking back to the seabed at the northern Gulf of Mexico site (about 30 miles NE of Macondo) and, further, that the concentration of organic carbon (which might or might not be oil related) in this material increased with time, too.  Two questions then arose that we could not answer from those results alone:

1)    Were the increases in mass and carbon flux in 2010 different from what would be expected in the Gulf of Mexico anyway in Spring and Summer where, (just as happens on land after Winter) increased hours of daylight and warmer temperatures can lead to a sudden flourishing of life in the surface ocean, which can also lead to an increase in the fall of waste material to the seafloor?

2)    Whether the results observed at the time of the DWH accident were typical or atypical, did they carry any distinctive geochemical signatures that might allow us to “fingerprint” them as being related to the oil spill?

 In continuing work we have made important progress.  By completing similar studies in 2011 we showed that the total amount of material and the carbon content of that material sinking to the same site over the Spring/Summer cycle of 2011 was not significantly different from that of 2010.  However, in one measurement that can be made in my laboratory it was found that, by comparing the ratio of carbon [C] to nitrogen [N] in the sinking material, the highest material flux samples with the highest carbon contents at the height of the DWH accident in 2010 appeared to be composed of signific...

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