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11th ICRS Abstract book - Nova Southeastern University

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Poster Mini-Symposium 17: Emerging Techniques in Remote Sensing and Geospatial Analysis<br />

17.553<br />

GIS Derived Spatial Analysis as a Tool to Predict Nearshore Coral Reef Fish<br />

Species in American Samoa<br />

D. Paul BROWN* 1 , Gerald ALLEN 2<br />

1 National Park Service, Pago Pago, American Samoa, 2 Department of Aquatic Zoology,<br />

Western Australian Museum, Perth, Australia<br />

The U.S. National Park Service has undertaken a monumental task of inventorying<br />

species found within park boundaries both below water and on land. This is part of the<br />

Inventory & Monitoring program aimed to increase our management efforts in all the<br />

U.S. National Parks. In the National Park of American Samoa, the inventory of coral reef<br />

fish has helped to discover 44 new species records for the territory of American Samoa.<br />

This was done using both GIS polygons derived from known geographic distributions of<br />

marine fish as well as in-water surveys using SCUBA and technical diving procedures. A<br />

distribution map was created for all known coral reef fish species from the central South<br />

Pacific. Using ArcInfo GIS software, a point was generated on an equal area map of the<br />

South Pacific for each recorded occurrence of a given species. These point records,<br />

whether collection or observational records, were then used to create a GIS polygon.<br />

Although these polygons include broad expanses of deepsea/ pelagic habitat, it is<br />

assumed that fish species only occur in suitable habitat. When American Samoa fell<br />

inside this polygon, it was assumed that this species could be found. GIS benthic habitat<br />

maps were then used to locate suitable and likely locations for a given species. In-water<br />

surveys were then conducted to look for the assumed present species. Using this<br />

technique 118 additional species were presumed to be located in Am. Samoa. To date the<br />

in-water surveys have found 44 new records, of these, 27 were assumed present from the<br />

GIS modeling but had never previously been found. Many of the remaining species are<br />

small and cryptic and are unlikely to be encountered without the use of icthyocides.<br />

17.554<br />

Monitoring The Health Of Coral Reef Using Multi-Temporal Remote Sensing -A<br />

Case Study Of Pirotan Island, Marine National Park, Gulf Of Kachchh, Gujarat ,<br />

India<br />

Sahadev SHARMA* 1 , Anjali BAHUGUNA 2 , Nandini Ray CHAUDHARY 2 , Shailesh<br />

NAYAK 3 , Sachin CHAVAN 4 , Chavi Nath PANDEY 4<br />

1 <strong>University</strong> of the Ryukyus, Okinawa, Japan, Nishihara, Japan, 2 Space Applications<br />

Centre (ISRO) Ahmedabad, India, Ahmedabad, India, 3 Indian National Centre for Ocean<br />

Information Service, Hyderabad, India, hyderabad, India, 4 Gujarat Ecological Education<br />

and Research Foundation, Gandhinagar, India, Gandhinagar, India<br />

Multi-temporal coral reef study is required for monitoring the climate and human impact<br />

changes. We have evolved an indicator-based (mainly satellite-derivable indicators)<br />

approach for monitoring health of reefs. The indicators tell about the damage already<br />

done, current ecological condition and early warning to the reefs. Early warning<br />

indicators are Sea Surface Temperature Anomaly, Turbidity, and Delay in Onset of<br />

Algae. The ecological indicators are diversity (both floral, faunal and habitat), percentage<br />

cover of live and dead corals, etc., and the Damage indicators are the deposition of mud<br />

and sand on the reef, erosion, phase shift, etc. The health status for Pirotan reef (22.6 0 N,<br />

70 0 E) located in the Gulf of Kachchh, India, has been assessed using health indicators.<br />

Indicators of Pirotan Reef health are temperature rise, high salinity, increase in macroalgae,<br />

over-fishing, high sedimentation rate, human influences, and deposition of mud<br />

over reef, etc. Indian Remote Sensing Satellite LISS III sensor data of periods 1998, 2000<br />

and 2005 were analysed to zone the eco-morphological zones of the reef like algal ridge,<br />

mud over reef, sandy muddy reef flat, live coral zone, seagrass, macro-algae, algae on<br />

muddy reef flat, etc. with an accuracy of 87% at 90% confidence level. NOAA-AVHRR<br />

average monthly SST data was analyzed from 1998 to 2005 (March, April, May and<br />

June) to identify the effect of temperature rise on coral reef like bleaching and increased<br />

macro-algae cover. Depositions of sand and mud have increased owing to the high<br />

sedimentation rate, sand mining and cutting of mangroves. Coral bleaching and stress has<br />

resulted in increased macro-algal growth. Onset of coral reef friendly macro-alga<br />

(Sargassum) has shifted from September-October to early December. The Pirotan reef is<br />

under severe degradation as is apparent from the indicators of health. Efforts are currently<br />

underway to model the indicators for establishing health.<br />

17.555<br />

Coral Color - Reflection And Absorption<br />

Noga STAMBLER* 1<br />

1 Life Sciences, Bar Ilan <strong>University</strong>, Ramat Gan, Israel<br />

Light absorption per unit of coral surface area decreased with increase in colony size, with a<br />

clear effect of different coral morphologies. In branched colonies, shading among branches<br />

reduced the absorbed light per unit area and per zooxanthellae.<br />

Corals often have different colors; color is variable, even among colonies of the same species<br />

growing together. While the colors blue, pink, and green are due to the protein pigments in the<br />

host tissue, the brown color is due to the absorption of the zooxanthellae pigments.<br />

Coral colors change as a result of acclimation and adaptation to environmental conditions. Dark<br />

brown colors, representing higher absorption, are due to low-light intensities or exposure to<br />

high-nutrient concentration, while lightness colors are due to low pigment concentrations, in<br />

some cases due to natural conditions while others indicate stress conditions.<br />

The absorption range of the corals and their symbiotic zooxanthellae, and their ability to change<br />

their color by photo-acclimation and photoadaptation enable the coral to grow and survive.<br />

These variations can monitor on a reef level, however corals can exhibit different colors in the<br />

same colony. The spectral variation between color morphs of the hermatypic corals Stylophora<br />

pistillata and Pocillopora damicornis in the northern Red Sea was found to be higher than<br />

between species. Therefore species recognition based on reflectance spectra is only possible in<br />

certain cases.<br />

17.556<br />

Geomorphological Symbolization Of Coral Reef Environments Along The Southeast<br />

Coast Of Florida: Interpretation Of Airborne Laser Bathymetry And Development Of An<br />

Extension For Arcinfo GIS<br />

Jacob ESTEBANELL BECERRA 1 , Victoria ACHATZ 2 , Charles FINKL* 3<br />

1 Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain, 2 School of Geoinformation,<br />

<strong>University</strong> of Applied Sciences Villach, Villach, Austria, 3 Coastal Geology & Geomatics,<br />

Coastal Planning & Engineering, Boca Raton, FL<br />

Interpretation of laser airborne depth sounding (LADS) imagery along the SE Florida coast<br />

initially identified numerous coral reef environments that were displayed as discrete polygons<br />

on maps. Although this recognition of morphoforms provided a comprehensive overview of<br />

spatial differentiation and interrelationships between reef subsystems, the topology lacked clear<br />

integration of form with function and morphodynamic processes. In an effort to glean more<br />

information from the LADS imagery that would better reflect the detailed distribution of<br />

morphoforms, we amalgamated symbolization as recommended in manuals for meso- and<br />

microscale geomorphological mapping as seen in the Geomorphological Map of Europe. The<br />

procedure involved detailed subdivision of mapping units already derived for the 600 km2<br />

study area by interpretation of morphoforms and onscreen digitizing using symbols specifically<br />

created for this purpose. The characterization of coral reef environments involved classification<br />

of different geomorphic forms and processes followed by the creation of index forms for maps.<br />

After adapting existing landscape symbols to seafloor forms and adding new symbols, hand<br />

drawn maps including all patterns (point, line, polygon) were prepared as overlays to the LADS<br />

imagery. Polygon and point patterns were digitized in a graphics drawing program while line<br />

patterns were created in the ArcGIS Style Manager. After importing geomorphic symbols into<br />

the ArcGIS Library, shape and color patterns were adjusted for final digitalization of the<br />

geomorphic map with a self programmed extension for ArcGIS. The result produced maps<br />

showing coral reef environments displayed in terms of true geomorphic symbolization.<br />

402

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