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Personnel: Dr. Frank Kinnaman, Dr. Susan Mau, Blair Paul, Monica Heintz, Christopher Farwell. Assessing the Efficacy of the Aerobic Methanotrophic Biofilter in Methane Hydrate Environments. Principal Investigator: David L. Valentine, UCSB
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Personnel: Dr. Frank Kinnaman, Dr. Susan Mau, Blair Paul, Monica Heintz, Christopher Farwell.

Assessing the Efficacy of the Aerobic MethanotrophicBiofilter in Methane Hydrate Environments.

Principal Investigator: David L. Valentine, UCSB

Overarching Goal• Assess the importance of methanotrophy

in preventing the escape of marine methane from hydrate and related reservoirs to the atmosphere.

Outline• Background• Objective 1: Impact of mats on flux• Objective 2: Regional SBB CH4 budget • Objective 3: Methanotrophic controls• Schedule• Milestones

Marine Methanotrophic Biofilter

Marine CH4 Reservoir

Anaerobic Oxidation

Aerobic Oxidation

Deep Subsurface

70-300 Tg y-1

5-20 Tg y-1

~5 Tg y-1 Atmospheric Flux

Shallow Subsurface

Ocean

Atmosphere

5×1017 – 1×1019g

Background

Two Biofiltration RegimesAerobic

CH4 + 2O2 CO2 + 2H2OCH4 + 2O2 CO2 + 2H2O

AnaerobicCH4 + SO4

2- HCO3- + HS- + H2OCH4 + SO4

2- HCO3- + HS- + H2O

5 µm

Boetius et al. 2000

Background

Objective 1

• Determine the impact of benthic microbial mats on methane flux from the subsurface into the ocean. Specifically, identify methanotrophic organisms living in benthic mats at cold seeps, and quantify their capacity for methane oxidation.

Benthic Methanotrophs

H. Ding and D.L. Valentine Methanotrophic bacteria occupy benthic microbial mats in shallow marine hydrocarbon seeps, Coal Oil Point, CA. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, G01015, 2008.

Methanotrophs

Rule

Santa Monica Basin

Day 14 Day 21 Day 28 Day 35

Day 49 Day 56 Day 70 Day 77

Day 84 Day 91 Day 98 Day 105

In-situ Cultivation

In-situ Incubations

Proposed Experiments• Molecular analysis of mat communities, • Rate measurements to assess capacity

to oxidize CH4,• Isotope probing experiments to directly

assess the cellular uptake of CH4.

Early Results13C-DNA Yield

0

50

100

150

200

250

1.398 1.400 1.402 1.404 1.406 1.408 1.410

Density (ng/ul)

DN

A O

btai

ned

(ng)

13C12C

Potential Impact• Potential to reveal the identities and

importance of benthic communities in moderating the flux of methane from the subsurface to the ocean.

Objective 2• Develop a regional methane budget for

a classic marine environment containing methane hydrates and cold seeps – the Santa Barbara Basin.

Surf

ace

Wat

ers

Santa Barbara Basin CH4 Budget

COP Seeps

A.

A.

C. D.

..

.E.

Santa Barbara Basin

Preliminary Budget: COP Plume

COP

Tran

sect

4

Tran

sect

3

Tran

sect

2

Tran

sect

1HC6

HC7

HC8 HC9

HC10

HC11 HC12

HC13

HC14 HC15

HC16

HC17

Preliminary Budget: COP Plume

-120.2-120.25-120.15 -120.1 -120.05 -120 -119.95

34.3534.36

34.3734.38

34.3934.4

34.4134.42

34.43

0

50

100

150

200

250

300

350

400

Longitude

Latitude

Dep

th (m

)

HC8

HC7

HC6

HC9

HC10

HC11

HC14

HC13

HC12

HC15

HC16

HC170.3 m/s

Current Velocity Distributions

Oxidation rate = Concentration × Fraction oxidizedOxidation rate = Concentration × Fraction oxidized

Experimental Approach:Methane Oxidation Rate MeasurementsExperimental Approach:

Methane Oxidation Rate Measurements

C*H4 + 2O2 CO2 + 2*H2O C*H4 + 2O2 CO2 + 2*H2O MethanotrophsMethanotrophs

Inject tracerInject tracer

IncubateIncubate Spargeunreactedmethane

Spargeunreactedmethane

Count radioactivity in the sample

Count radioactivity in the sample

Water Column

Potential Impact• A closed methane budget for the SBB

will provide a critical case study on the efficiency of the methanotrophicbiofilter for preventing methane release to the atmosphere.

Objective 3• Determine the primary controls on

aerobic methane oxidation in marine waters overlying environments with methane hydrates and cold seeps.

Study Sites

COP Seeps

ERB

SBBSMB

SMB

SCB?ETNP

Proposed Experiments• Methane Concentrations • Methane Oxidation Rates• Compare against:

– Depth, Oxygen, Illumination, Water mass history, Circulation, Basin restriction, Proximity to shore, and other Environmental factors.

Potential Impact• Quantitative relationships between

environmental conditions and methane turnover can be used to predict the potential of marine methane to escape into the atmosphere, and will feed important parameters into carbon cycle models

Schedule2009 2010 2011

Water Sampling COP SEEPS 09 COP/SBB

Mat Sampling COP SMB

Mat Analyses COP/SIP SMB/SIP

CH4 Analyses COP SEEPS 09 COP/SBB

CH4 Budget SMB? COP/SBB

Phylochip COP/SBB

Sampling COP SEEPS 09 COP/SBB

Analyses COP SEEPS 09 COP/SBB

Objective 1

Objective 2

Objective 3

Targets of Opportunity: Phylochip, AK lakes (Ice & Ice-free), San Clemente Basin, ETNP

Milestones• Milestone 1: Successful installation and sea trial of the CTD

rosette system and ADCP. 4/1/09. • Milestone 2: Confirmation of 3H-CH4 oxidation and 13C-CH4uptake by benthic microbial mats from Coal Oil Point seeps.

7/1/09.• Milestone 3: Completion of the SEEPS 09 cruise. Estimated

completion date for this milestone is 1/1/10, but the timing will necessarily depend on the UNOLS scheduling. Currently scheduled Aug 27 – Sep 15, 2009.

• Milestone 4: Conduct a preliminary analysis for mmo and 16SrRNA gene sequences for putative methanotrophs from the Santa Monica Basin, and compare to sequences from Coal Oil Point seeps. 7/1/10.

• Milestone 5: Complete a preliminary analysis of current velocity data and oxidation rate data from the SEEPS 09 cruise. 10/1/10.

• Milestone 6: Complete the ocean-going sampling program, and perform preliminary analysis of all physical and chemical data to ensure sufficient data for further analysis. 4/1/11.


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