Title: Benthic Ecology from Space
1Benthic Ecology from Space
- Heidi Dierssen, Univ. CT
- Richard Zimmerman, Old Dominion
2Acknowledge
- Univ. CT
- Chris Buonassissi
- Dirk Aurin
- Alison Branco
- Old Dominion Univ.
- David Burdige
- Lisa Drake
- Victoria Hill
- David Ruble
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4Questions
- How much do the shallow carbonate sediment banks
contribute to NPP? - How do seagrasses on these banks influence the
carbon cycle (carbonate dissolution) and heat
budgets? - What are the mechanisms underlying seagrass
distributions?
5Moving Beyond Qualitative
- Qualitative maps
- Presence or absence of benthos
- cover
- Quantitative maps
- Leaf area index (LAI) m2 m-2
- LAI or standing crop to NPP
- LAI to Carbonate dissolution
- Bottom albedo for heat budgets
6Biomass to benthic NPP
7Carbonate Sediment Geochemistry
- Seagrasses oceanic sink for carbon
- Shallow water biological pump
- Decomposition in sediments
- Carbonate sediment dissolution
- Burdige Zimmerman, Limnol. Oceanogr. 2002. 47
1751-1763
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9Comparing two sites
- 1) Bahamas Banks
- Little anthropogenic influence
- Constant water column IOPs
- Primarily ag, whitings
- 2) Florida Bay
- Anthropogenic disturbance
- CDOM, sediment, and phytoplankton
10Seafloor Measurements
- Bottom reflectance
- DOBBS
- Seagrass quadrats
- Seagrass primary productivity
- Digital camera/strobe
- Sediment cores
- Reflectance
- Particle size spectrum
- Chl, PP
- Seagrass blades
- Morphometrics
- Reflectance
11Water column
- ac-9 package, eco-VSF, CTD, fluorometers (Chl,
CDOM, phycoer.) - Hydroscat 6
- LISST 100X, particle size analyzer
- Irradiance
- Planar, Ed (2 depths), Eu over substrate
- Scalar Eod (2 depths), Eou
- Filtered for TSM, Chl, CDOM
12Sea surface interface
- Remote sensing reflectance
- HyperPro
- Analytical Spectral Devices (ASD)
- Data available at http//colors.uconn.edu
13Intensive Field work
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15Field Work
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1624 ft. boat
17Lesson 1 Sediment Reflectance is highly variable
18Lesson 2 Green color can be seagrass OR sediments
19Seagrass
Island Shadow Effect
LAI (m2 m-2) Land 0 0.38 0.75 1.1 1.9 gt2.6
NPP (gC m-2 y-1) Land 0 100 200 300 500 gt700
Area 78,000 km2 Mean 1.4, 360 g C m-2
y-1 Integrated 2.8 x 1013 g C y-1
201998
1999
21Approaches
- Use known bathymetry
- Time as another variable
- More spectral channels
22Lesson 3 Need total ecosystem productivity
Above-ground NPP 2.8 x 1013 g C y-1
Benthic Microalgae (10-100 mg Chl m-2)
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Below-ground NPP
Leaf epiphytes
Phytoplankton, 1 (0.12 mg Chl a m-3)
23Lesson 4 Need to understand fate of production
- Carbonate dissolution
- Assumes seagrass blades decompose in sediments
- 2 of annual oceanic CO2 uptake
24FL Bay seagrass beds have little debris Export
Carbon out of system
25Lesson 5 Avoid hurricane season
Post-Hurricane Wilma 2005
26Jan 2006
27Atmospheric Correction
Atmospheric Correction
28Current Collaborators
- Atmospheric Correction
- TAFKAA model (Bo-Cai Gao)
- Hyperspectral imagery, Paul Bissett FERI
- Total suspended matter, GOBI Model, Mike
Twardowski - Air-Sea CO2 Flux, Wade McGillis
- Carbonate dissolution, David Burdige
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