DYNAMIC VARIABILITY IN THE SPECTRAL-POLARIZED LIGHT FIELD MEASURED OVER SEAGRASS AND SAND HABITATS Russell, Brandon1; Dierssen, Heidi1, R.C. Zimmerman2 1 Department of Marine Sciences/Geography, University of Connecticut, Groton, CT 06340, USA Department of Ocean, Earth & Atmospheric Sciences, Old Dominion University, 4600 Elkhorn Ave., Norfolk VA 23529, USA Brandon.russell@uconn.edu 2 INTRODUCTION Biological camouflage has evolved in multiple phyla as an adaptation to visually-orienting predators. (Hanlon 2009, Claes 2010, Hacker 1991) Underwater, the light field is polarized to a much greater and more complex degree than in terrestrial environments. The ability to detect and utilize polarized light for vision is present in a large number of marine animals. (Chiou 2008, Shashar 2000, Cronin 2003, Mathger 2006) Organisms may change their polar spectral reflectivity to minimize their contrast to their environment and thereby avoid detection. Here, we present measurements of the dynamic and complex light field in the nearshore, coastal environment as a foundation for exploring the underlying camouflage mechanisms of select species of fish found in these habitats. Spectral polarized light and reflectance measurements were made in waters near Port Aransas, Texas in June 2010. Two habitats were explored: 1) seagrass meadows, habitat for the dynamically camouflaging pinfish; and 2) sandy sediment, habitat of the southern flounder. Benthic reflectance spectra from these two environments are presented, as well as simultaneously recorded polarized measurements. Additionally, polarized spectra from two local species of seagrass were compared to floating macroalgae (Sargassum sp.). These field and laboratory measurements will serve as parameters for light-field modeling and laboratory organismal studies, as well as facilitate interpretation of the dynamic camouflage mechanisms specific to organisms dwelling in these different habitats. METHODS Research was based at the University of Texas, Marine Science Institute in Port Aransas, TX. Work was conducted between June 14 and 25, 2010 using the R/V Shearwater. Field spectral measurements presented here were taken at a sheltered location (27° 48.644’N, 97° 7.147’W) in the lee of Mustang Island, Chorpus Christi Bay on June 18, 2010. In-situ hyperspectral measurements were made of seagrass canopies and sandy sediment bottoms using Satlantic HyperOCR radiometers from a Hyperspectral Tethered Spectroradiometer Buoy (HTSRB) package, measuring Lu at a frequency of1Hz. Sensors were fixed to a hand-held wand for measurements normal and 45° to the substrate. Interchangeable plastic polarization filters (Alight) were attached to the fore-optics for polarization measurements. Linear, right circular, and left circular filters were used. Sensors were held 3cm from the target surface. Polarized measurements were coupled with simultaneous downwelling and upwelling plane irradiance measured by the Diver Operated Benthic Bio-Optical Spectrometer (DOBBS), consisting of a HydroRad-4 radiometer system (HOBI Labs). The two plane irradiance sensors measuring Ed and Eu were mounted to an adjustable wand and positioned just above the target surface. In addition to field measurements, locally collected specimens of Thalassia testudinium, Halodule wrightii, and Sargassum sp. were analyzed in the laboratory for reflectance of both linearly and circularly polarized light. Linear vertical, linear horizontal, linear 45°, and left and right circular polarization orientations were examined. Lab measurements were carried out using an ASD FieldSpec radiometer in a darkened room. The illumination source was positioned 0.7m above the specimens. Plant samples and 99% spectralon reference were placed on a matte black surface, under 6cm seawater. The fiber optic probe was held, submerged, 1cm from the target and at 45° to vertical, 90° from the plane of illumination. Polarization filters were held perpendicular and in contact with the probe. Spectra were averaged over 5 samples. PRELIMINARY RESULTS OF MEASUREMENTS MADE IN THE FIELD (Fig. 1-3) AND LAB (Fig. 4-6) In-situ DOBBS measurements of T. testudinium canopy and sandy benthos. (Fig. 1) In-situ HTSRB measurements of T. testudinium canopy and sandy benthos using polarization filters. (Fig. 2) Reduction of light intensity through polarization filters over T. testudinium canopy and sandy benthos using HTSRB. (Fig. 3) Laboratory FieldSpec measurements of T. testudinium, H. wrightii, and Sargassum sp. Spectra measured through polarization filters were normalized to filtered measurements of spectralon reference standard. (Figs. 4, 5, 6) At the location and time of field measurements, LISST data shows a particulate concentration of approximately 60micro-liters/liter, most being in the 45-100 micron range, and Kd approximately 4 over the spectral range used here. Seagrass and Sand Reflectance R b (dimensionless) 0.12 Sand 0.1 0.08 0.06 0.04 Seagrass 0.02 0 400 450 500 550 600 650 700 750 Wavelength (nm) Figure 1. Reflectance of Thalassia canopy and sand measured at 15 cm above seafloor with the Diver operated benthic spectrometer (DOBBS). Ambient Spectra, Thalassia and Sand 2.5 2 Seagrass No Filter (uW/cm^2/nm/sr) Sand No Filter 1.5 Seagrass Linear Sand Linear Seagrass L Circ Sand L Circ 1 Seagrass R Circ Sand R Circ 0.5 0 400 450 500 550 600 650 700 750 Wavelength (nm) Figure 2. Ambient light field at seagrass canopy and sand at 3cm from target with Hyperspectral Tethered Spectroradiometer Buoy Lu sensor. Ambient Light Reduction 0.7 0.6 Relative Intensity 0.5 0.4 Seagrass Linear Sand Linear Seagrass L Circ Sand L Circ Seagrass R Circ Sand R Circ 0.3 0.2 0.1 0 400 450 500 550 600 650 700 750 Wavelength (nm) Figure 3. Intensity of ambient light over seagrass canopy and sand through polarization filters, relative to unfiltered measurements. Light intensity from both is reduced to between 40% and 60% when passed through any filter. Thalassia Reflection Normalized to Reference 0.16 0.14 Relative Reflection 0.12 0.1 No Filter Vert Horiz 45 Deg L Circ R Circ 0.08 0.06 0.04 0.02 0 450 500 550 600 650 700 Wavelength Figure 4. Relative reflection of different orientations of polarized light for T. testudinium. Halodule Reflection Normalized to Reference 0.16 0.14 Relative Reflection 0.12 0.1 No Filter Vert Horiz 45 Deg L Circ R Circ 0.08 0.06 0.04 0.02 0 450 500 550 600 650 700 Wavelength Figure 5. Relative reflection of different orientations of polarized light for H. wrightii. Sargassum Reflection Normalized to Reference 2 1.8 1.6 Relative Reflection 1.4 No Filter Vert Horiz 45 Deg L Circ R Circ 1.2 1 0.8 0.6 0.4 0.2 0 450 500 550 600 650 700 Wavelength Figure 6. Relative reflectance of different orientations of polarized light for Sargassum sp. ACKNOWLEDGEMENTS This work was supported by a grant from the Office of Naval Research Multi-University Research Initiative. We wish to thank the faculty and staff of UT MSI, as well as our colleagues conducting simultaneous research who rendered assistance. REFERENCES Chiou, TH, Klienlogel, S, Cronin, T, Caldwell, R, Loeffler, B, Siddiqi, A, Goldizen, A, Marshall, J. 2008. Circular polarization vision in a stromatopod crustacean. Curr. 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