Mapping Potential Spawning Substrate for Shortnose and Atlantic Sturgeon in Coastal Plain Rivers of Georgia Using Low-Cost Side-Scan Sonar

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Mapping Potential Spawning Substrate for Shortnose and Atlantic Sturgeon in Coastal Plain Rivers of Georgia Using Low-Cost Side-Scan Sonar Mapping Potential Spawning Substrate for Shortnose and Atlantic Sturgeon in Coastal Plain Rivers of Georgia Using Low-cost Side-scan Sonar Thomas L. Litts, Georgia Department of Natural Resources, Wildlife Resources Division, 2065 Highway 278 SE, Social Circle, Georgia 30025 Adam J. Kaeser, U.S. Fish and Wildlife Service, 1601 Balboa Avenue, Panama City, FL 32405 Abstract: Characterizing the habitat of large, navigable rivers is difficult, yet this information is critically important to the conservation of a variety of resident aquatic species. We used low-cost sonar habitat mapping to map benthic substrates throughout nearly 1000 km of four Coastal Plain rivers in Georgia and to quantify the distribution of rocky substrates that may serve as potential spawning habitat for two imperiled sturgeon species, the shortnose sturgeon (Acipenser brevirostrum) and the Atlantic sturgeon (Acipenser oxyrinchus). Although we identified hard, rocky substrates in roughly half of the river km suggested by previous researchers as potential spawning zones, mapping revealed hard substrates in many other locations as well. Our approach provided a detailed view of the distribution, configuration, and extent of these habitats across the riverscape; these results can be used to support future research to gain a better understanding of other key factors associated with spawning habitat selection and habitat change over time. The ability to train novice technicians to execute all phases of the mapping process, and the overall classification accuracy achieved (82%) in this study demonstrated the practicality of this methodology for providing the spatially explicit, and continuous perspective of habitat required for effective con- servation across the freshwater range of migratory species like sturgeon. Key words: Acipenser brevirostrum, Acipenser oxyrinchus, spawning, habitat distribution, GIS Journal of the Southeastern Association of Fish and Wildlife Agencies: 3:80–88 Characterization and assessment of habitat is challenging in and habitat conservation (National Marine Fisheries Service 1998, large and turbid river systems inhabited by sturgeon and other 2012). Moreover, such information is critical to a variety of legal imperiled aquatic species, yet this information is fundamental to mechanisms associated with species conservation under the En- conservation success. Several coastal plain rivers of Georgia are in- dangered Species Act, such as Section 7 consultation and Section 4 habited by two federally-protected species of sturgeon, the endan- recovery (U.S. Fish and Wildlife Service 1973). gered shortnose sturgeon (Acipenser brevirostrum), and the en- Until recently, production of high-resolution maps of classified dangered South Atlantic population segment of Atlantic sturgeon benthic substrates and other habitat features over large spatial ex- (Acipenser oxyrinchus; National Marine Fisheries Service 1998, tents in inland freshwater systems was logistically impractical, and 2012). As anadromous fish, adult sturgeon migrate from estuaries thus infrequently conducted, due to expense and technical require- into freshwater rivers seeking rocky or coarse substrates such as ments. Between 2006 and 2008, the Georgia Department of Natu- gravel, cobble, boulder, and bedrock to deposit their adhesive eggs ral Resources (GADNR) pioneered a methodology for producing during spawning (Hall et al. 1991, Collins et al. 2000, Schueller and such maps using the inexpensive (~US$2500) Humminbird Side Peterson 2010). Within Georgia, shortnose sturgeon ascend rivers Imaging system, a recreational-grade, side scan sonar device (Kae- during winter to presumably spawn in the spring; whereas Atlantic ser and Litts 2008, 2010). Sonar imaging of entire river channels is sturgeon enter rivers either in spring or late summer to presum- possible with this equipment, and interpretation of imagery allows ably spawn in the fall (Peterson and Ingram 2015). Although the for the delineation and classification of major substrate classes and availability of clean, hard substrates is essential to spawning suc- the mapping of large woody debris, river banks, and other key fea- cess, coastal plain rivers of Georgia are typically predominated by tures within a geographic information system (GIS) environment. sandy substrate, and patterns of fine sediment deposition are dy- Methods for riverine habitat mapping were successfully demon- namic and influenced by hydrologic regimes and regulation, chan- strated and validated on ~200 km of rivers and creeks in southwest nel alteration, and land-use practices that affect sediment inputs Georgia (Kaeser and Litts 2008, 2010; Kaeser et al. 2012). The suc- and sediment transport (Garman and Nielsen 1992, Watters 1999). cess of these efforts suggested that low-cost sonar habitat mapping Thus, the ability to identify and quantify potential spawning sub- might be used to characterize benthic habitats throughout entire strates, and to monitor changes in the availability and condition of river basins, providing both the high spatial resolution necessary these habitats over time, is an essential element of species recovery to identify discrete patches of suitable spawning substrate for stur- 2016 JSAFWA 80 Sonar Mapping Sturgeon Habitat in Georgia Rivers Litts and Kaeser 81 impoundments is not possible; therefore, the barriers represent the upper limit to sturgeon migrations. The Ocmulgee and Oconee rivers join to form the Altamaha River, which flows unobstructed to the Atlantic Ocean. This study targeted the free flowing portions of each river, beginning below the most downstream impound- ments where navigation was feasible (e.g., North Macon Shoals on the Ocmulgee River) and concluding at Altamaha River Park on the Altamaha River and the I-95 bridge across the Savannah River. Survey end points were selected for practical reasons associated with river widening and braiding in lower reaches and the notion that additional spawning substrate would not be found further downstream. Sonar Survey and Data Processing To identify and plan sonar surveys, we first mapped all acces- sible boat ramps, calculated inter-ramp distances, and identified river segments (25–50 km) that could be surveyed in a day. Opti- mal flows for surveys that permitted safe navigation and provided full inundation of river channels were identified by reviewing hy- drographs and consulting with biologists familiar with study river Figure 1. Map of the study area and accuracy assessment reach locations on the Altamaha, Ocmul- reaches. The majority of sonar survey work on the Ocmulgee, gee, Oconee, and Savannah rivers in Georgia. Oconee, and Altamaha rivers was completed between December 2010 and April 2011. The Savannah River was surveyed the fol- geon and the large-scale spatial coverage required to quantify these lowing year during March and April 2012; additional survey de- patches across the vast reaches of river traversed by migratory fish. tails can be found in the final project report (GADNR 2013). All Thus, the objective of this study was to characterize and quantify surveys were conducted downstream at a pace of ~8 km h –1 using potential shortnose sturgeon and Atlantic sturgeon spawning sub- a Humminbird 1198c SI system, with a front-mounted transduc- strate across ~950 km of the Altamaha, Ocmulgee, Oconee, and er. The transducer was attached to a galvanized pipe, mounted at Savannah rivers in Georgia. The distribution of rocky substrates the front of a powered 5-m long johnboat using a trolling motor revealed by sonar mapping was compared to suggested spawning mounting bracket, and was set ~10–13 cm below the river surface. zones identified through previous telemetry investigations of stur- The SI system was networked to WAAS-enabled Garmin GPSMAP geon in the Altamaha and Savannah rivers. 76 GPS to provide coordinate data at image capture locations and a series of track points representing the survey path and associated Methods depth observations at 3-sec intervals. The GPS antenna was po- Study Area sitioned near the transducer to maximize image capture location Three of the study rivers, the Altamaha, Ocmulgee, and Oconee, accuracy. Sonar imagery was collected as a series of consecutive flow entirely within the state of Georgia; whereas, the Savannah overlapping screen snapshots. All rivers were surveyed using an River forms the boundary between Georgia and South Carolina operating frequency of 455 kHz and sonar range settings between for much of its course (Figure 1). The headwaters of the Ocmulgee, 27 m and 49 m, selected to optimize image resolution relative to Oconee, and Savannah rivers originate above the “Fall Line,” a geo- average channel width and depth (Fish and Carr 1990). Whenever logic feature oriented northeast to southwest across the middle of channel width exceeded a maximum swath width of 98 m per side, Georgia that represents the boundary between the Piedmont and a multi-pass, parallel-transect survey approach was employed to Coastal Plain ecoregions (Wharton 1989). The Ocmulgee, Oconee, maintain high image resolution across the river channel and mini- and Savannah rivers are each impounded at multiple locations; the mize unclassified areas of the channel (Kaeser et al. 2012). most downstream impoundment on each river is the Juliette Low- Sonar image geoprocessing was conducted according to meth- head Dam, the Sinclair Dam, and the New Savannah Bluff Lock ods described in Kaeser et al. (2012) but adapted for ArcGIS 10.0. and Dam, respectively (Figure
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