Stonecat Abundance and Population Parameters in Vermont’s Missisquoi and LaPlatte Rivers. Masters Proposal Betsy Puchala Advisor Dr. Donna L. Parrish Rubenstein School of Environment and Natural Resources Aquatic Ecology and Watershed Science Justification Stonecats (Noturus flavus, Rafinesque 1818) are listed as endangered in the state of Vermont (Langdon et al. 2006). In November 2008 lapriside (TFM) was applied to the Missisquoi River at Swanton dam (Cox 2009). At the completion of the 2008 treatment 36 stonecats where found stressed and 22 dead (Cox 2009). TFM is a chemical applied to streams and tributaries in order to control larval populations of sea lamprey, an invasive species that has detrimental effects on game fish populations (Brege et al. 2003). The lampriside treatments in the Missisquoi River occurs every four years, and is essential to the continuing success of the salmon stocking program. With the death of an endangered species it became important to learn more about the stonecat’s population parameters, such as age class structure, birth and death rates, in Vermont. This information is critical in managing and understanding the current and future populations of stonecats in Vermont. While this study will not address all population parameters it will address population abundance, habitat use, age class structure, and sex ratio. Objectives Estimate the abundance of stonecats in the Missisquoi River above and below Swanton dam. Estimate the abundance of stonecats in the LaPlatte River above and below Shelburne Falls. Determine seasonal movement, and habitat use, for stonecats in Missisquoi River. Map substrate in the Missisquoi River above and below Swanton dam to determine suitable habitat for stonecats. Determine the age class structure and sex ratio of stonecats in the Missisquoi and LaPlatte Rivers. Background Abundance Stonecat (Noturus flavus, Rafinesque 1818) is the only Noturus species found in Vermont and is listed as endangered by the Vermont Fish and Wildlife (Langdon et al. 2006). Their known range in Vermont is limited to the LaPlatte and Missisquoi Rivers, including Hungerford Brook, a tributary to the Missisquoi River (Cox 2009; Langdon et al. 2006). Stonecats are found 2 throughout the United States from Montana throughout the Mississippi basin including Oklahoma and Alabama and reaching into southern provinces of Canada including Alberta, Manitoba, Quebec, and Ontario, see figure 1 (McCulloch and Stewart 1998; Pollard 2004). Vermont lays in the eastern most part of its range. The abundance of stonecat in Vermont is unknown, and have only been documented in the two rivers described above. Stonecats are rather common throughout the rest of its range and are not listed for any type of federal protection. There are some locations, Alberta Canada, Mississippi, Tennessee and Virginia, where the stonecat is in need of conservation but is not legally enforced as seen in Vermont (Mississippi Museum of Natural Science 2005; Pollard 2004; Tennessee aquatic nuisance species task force 2008; Virginia department game and inland fisheries 2010). There could be a number of reasons why stonecats are in need of conservation and it varies depending on the location. Much comes from habitat destruction (Langdon et al. 2006; Sindt et al. 2011), but there are other sources such as siltation (Langdon et al. 2006; Trautman 1957), or temperature limitations at the edges of their range (Kline and Morgan 2000; Pollard 2004). Habitat Little information is known about habitat preferences for stonecats. Stonecats utilize a wide range of habitat including, pools, the main channels of the Mississippi, Ohio and Missouri Rivers, and even rocky lake shores as seen in Lake Erie (Gilbert 1953; Langdon et al. 2006; Layher and Wood 1986; Walsh and Burr 1985). While they have been observed in many types of macrohabitats they are most often seen in riffle type areas, with a relatively swift current and shallow depth (Banks and DiStefano 2002; Kline and Morgan 2000; Layher and Wood 1986; McCulloch and Franzin 1996). Most often stonecats are sampled in locations where the current is less than 1 meter per second and depths less than 1 meter. Table 1 shows a summary of depth (m) and velocity (m/s) where stonecats have been observed. Stonecats prefer areas with cover. They hide in crevices often between boulders, and have even been observed burrowing into gravel (Steiner 2000). This is why their common name refers to stone (Steiner 2000). Stonecats are observed in all substrate types from silt to boulder, though they are most often found in rocky type substrate such as gravel and cobble, following 3 the Wentworth scale (Wentworth 1922). Table 2 shows a summary of percentage of substrate types where stonecats have been observed. The variation in substrate type and macrohabitat use may be due to seasonal movement. Other madtoms have been observed shifting habitats due to seasonality such as the nesho madtom where breeding adults were observed shifting to shallower areas (Bulger and Edds 2001). While there is no evidence of large distance movement, there is evidence of seasonal variation of habitat use (Brewer et al. 2006; Bulger and Edds 2001; Pollard 2004). The locations of stonecats at different times of the year will be essential knowledge with the ongoing lamrpiside treatments. Age Stonecats are the largest and latest to mature of the Noturus species. Males and female do not reach breading maturity until ages 3-4 (Walsh and Burr 1985). The largest stonecat on record came from Ohio at 312 mm (Trautman 1957), though most individuals from streams rarely live longer than 6 years and have a total length around 180 mm (Walsh and Burr 1985). In a study conducted by Gilbert (1953), it was found that stonecats from Lake Erie were larger on average than those found in streams in Ohio. It was postulated that they had greater access to food resources which allowed them to grow to larger sizes (Gilbert 1953). The stonecat is benthic and consumes mostly aquatic insects but also can eat mollusks, minnows and fish eggs (Langdon et al. 2006; Pollard 2004; Walsh and Burr 1985). Length of individuals is a common method for estimating age (Anderson and Neumann 1996). There appears to be a lot of overlap with length at age for individual stonecats (Gilbert 1953; Walsh and Burr 1985). Length and age information gives insight into future populations, because we are able to determine the number of spawning individuals as cohorts become mature. See table 3 for a summary of literature on stonecat lengths at age. Methods Study Site The study will take place in the Missisquoi and LaPlatte Rivers located in the Lake Champlain Basin, Vermont. Different types of landscapes, such as city, agriculture and forest, surround both rivers. The Missisquoi River originates in Lowell Vermont, it heads into Canada 4 for a few miles then comes back into Vermont in East Richford (Vermont agency of natural resources 2005). There are 7 dams located on the Missisquoi River the first in Troy Vermont and the last in Swanton VT. At least 6 of the dams, as of 2005, were still being used as hydroelectric facilities. Missisquoi River contains many habitat types. There are regions of riffle habitat in more abundance above the natural fall line, though some exist bellow Highgate and Swanton dams. Much of the river consists of deep slow moving water. LaPlatte River originates in Hinesburg VT, goes through Charlotte and Shelburne, and finally drains into Shelburne Bay, a potion of Lake Champlain (Winooski natural resources conservation district et al. 1979). The LaPlatte flows for approximately 16 miles and drains 36,740 acres of land (Winooski natural resources conservation district et al. 1979). There are no dams located on the LaPlatte River. Sampling Gear The rarity of stonecats and their ability to hide in crevices will greatly affect our ability to successfully sample for them. Because of this and the heterogeneity of the Missisquoi and LaPlatte Rivers, many methods will be used for sampling stonecats. Backpack electrofishing is a common method of sampling (Kline and Morgan 2000; Reynolds 1996; Westley and Fleming 2011) and will be used in wadeable areas. The amount time and area covered will be recorded at each sampling time. This technique is known to be effective for sampling stonecats (Cox 2009; McCulloch and Stewart 1998; Pollard 2004), but is time consuming, active, dependent on weather, stream discharge, and subject to bias of user experience. Minnow traps may also be used in wadeable and non wadeable areas. This has been used effectively on other Noturus species (Cox 2009; Knight et al. 2007) However, this method is rather time consuming, passive, and covers little area. Trap nets may be used in areas that are both wadeable and non wadeable. This method has work in capturing stonecats in the Missisquoi River at Hungerford Brook (Cox 2009), and may be used in other areas of the Missisquoi River if appropriate. Modified versions of trap nets that have been shown to be effective in capturing benthic fish (Crites et al. 2002; Gryska et al. 1998) may also be used, depending on success of other gear types. Mini Missouri trawl method will be used in both wadeable and non wadeable sampling areas. In wadeable sections the trawl will be pulled by hand and in non wadeable sections will be 5 pulled by boat. This has been shown to be effective on benthic fish species and has successfully captured stonecats (Herzog et al. 2005; Herzog et al. 2009; Neebling and Quist 2011). This is an active method, effective in pools, and river channels but less effective in riffle and rocky areas due to the net getting caught on the substrate. Tagging To be successful in grasping stonecat abundance and habitat movement individuals must be tagged. Regardless of the sampling gear used for capture, each individual will be marked with either a passive integrated transponder (PIT) tag, or a visible implant elastomer (VIE) mark. These two methods are commonly used on fish species (Guy et al. 1996; Hewitt et al. 2010; Hill et al. 2006). Tagging method will depend on the size of the individual, as a tag will not weigh more than 10% of any individuals body weight, and its location. PIT tags allow us to successfully keep track of individuals (Guy et al. 1996), as each tag has a unique number associated with it. This is essential for determining habitat movement throughout a season. When an individual is captured it will be anesthetized with MS222 at 100mg/L. The PIT tag will be inserted with a 10ml syringe and 12-gauge needle. A PIT tag requires recapture of an individual so that it can be read with PIT tag reader (Guy et al. 1996). A more recent advancement in technology has created PITpacks (Hill et al. 2006). These packs allow fish with PIT tags to be detected without having to be recaptured. The PIT tag reader has been modified to a ring that you use to scan for individuals much like a metal detector (Zydlewski et al. 2001). VIE has been shown to be effective both long term and on small endangered individuals (Phillips and Fries 2009). In the Phillip and Fries (2009) study VIE marking had no negative effects on growth, or survival. You cannot differentiate between individuals using a VIE tag, though large changes in movement will be detectable based on location where they were found. VIE marking does require recapture of individuals and handling time to visualize and confirm the VIE mark. Substrate Mapping Side scan sonar is often used in ocean systems for search and recovery efforts, and seafloor mapping. A similar method of using side scan sonar has come out of Georgia 6 Department of Natural recourses as an effective way to map substrate type in rivers (Kaeser and Litts 2008; Kaeser and Litts 2010). Substrate mapping will be used to determine potential stonecat habitat. This information will also help determine the location of sampling, to ensure that sampling is occurring in ideal stonecat habitat. A humminbird 1198c, which is a combination depth finder, mapping, and side scan sonar device often used by angles, will be used to map the substrate. The humminbird will be attached to the front of the boat. The boat will run downstream at approximately 5 mph and at designated intervals a snapshot of the substrate will be taken. The GPS location of each snapshot, waypoint, will be recorded along with the GPS coordinate path, track, that we will travel. The snapshot images will have to be rectified and then the waypoints and images will be joined, and finally placed along the track. This will result in a single image of the riverbed. I will create polygons on the images differentiating between substrate types. The result will be a vector layer that shows each substrate type and location. Movement There is no information on the movement of stonecats in Vermont. This will be accomplished by using the same gear types, during spring, summer, and autumn. The gear types will be placed in varying habitat types, (i.e. pools, riffles) and substrate types (i.e. gravel, sand). Keeping track of the individuals found in each location will indicate the kind of movement we can expect seasonally and it will also tell us the type of habitat stonecats are using. We will record the substrate type, temperature, and stream velocity with each capture period. Age Structure/ Sex Ratio Using otoliths and spines to age Icatlurides is a common method and has been successful with stonecats (Chan and G.R. 2000; DeVries and Frie 1996; Gilbert 1953; Maceina et al. 2007; Walsh and Burr 1985). Using otoliths are more accurate than spines, but requires sacrificing individuals (DeVries and Frie 1996; Maceina et al. 2007). It is illegal to kill stonecats in Vermont therefore stonecats will be sampled from the Great Chazy River, near Champlain New York, approximately 65 miles from the Vermont study sites. Roughly 200 stonecats will be captured at night using backpack electrofishing. Length, weight, and sex will be recorded for each individual. 7 Recording the sex of there 200 stonecats will tell us the sex ratio for stonecats in this region. In other Noturus species it has been observed to be a 1:1 ratio (Bulger and Edds 2001), but has not been reported for stonecats specifically. As with other Noturus species there is no sexual dimorphism displayed in stonecats except during spawning (Walsh and Burr 1985). Otoliths and right pectoral spine will be removed for ageing. Following procedures similar to Clugston and Cooper (1960) and Chan and Parson (2000) two people will examine each otolith and pectoral spine to determine age and precision between the two structures. This procedure will be done by two people to try and limit experience bias. Doing a comparison between structures will allow us to determine if taking spines, and which section of spines, could be a viable, non-lethal, method for determining stonecat ages in this region. There is little information that uses length to determine age for stonecats, and what is available is outdated and from other geographical areas (Gilbert 1953; Walsh and Burr 1985). To compare the length at age information from New York to that in Vermont, during sampling in the Missisquoi and LaPlatte Rivers length data will be taken for each individual. This will produce a length frequency histogram (Fuselier and Edds 1994; Simonson and Neves 1992) for Vermont stonecats. Length frequency histograms reflect age groups (DeVries and Frie 1996). Clustering of individuals at lengths will reveal cohorts. It can then be expected that each cohort reflects age groups and their expected length ranges. This histogram will add credence to the age class structure from the stonecats collected in New York without taking spines. Program MARK This robust program will allow us to create a model best suited to our data. We will use either the Jolly-Seber (open model) or Robust Design (combination open-closed model) to estimate population. Program MARK uses the number of individuals marked and recaptured during a designated amount of time to estimate total population. Necessary information such as fecundity will be obtained from the literature. Other information including age class structure and sex ratio will be the observed data from this study. Expected Results Substrate Mapping 8 A GIS layer describing the substrate type in the study sections of the Missisquoi and LaPlatte Rivers will be created. The area and location of each substrate type will be known and quantifiable (for an example see figure 2). Movement We expect to see stonecats captured in different areas of the river depending on the season. Specifically we hypothesize that stonecats are more likely to be in pools in early spring, shifting to shallow gravel beds during the breading season and into riffles during the summer as seen by Brewer et al. (2006) and Brewer and Rabeni (2008). Age Structure From the otoliths we expect to see a range of lengths that equate to age. We will know the precision of using spines to age stonecats compared to otoliths. We also expect a length frequency histogram from the Missisquoi and LaPlatte Rivers to compare to the age structure observed in the Great Chazy River. We will also know the sex ratio for stonecats in this region. Program MARK We expect to have population estimates for stonecat populations in the LaPlatte and Missisquoi Rivers. This information will include age structure, fecundity and birth and death rates obtained from the literature. Limitations One of the largest and most concerning limitations is the number of stonecats that we will be able to capture. The validity of program MARK and length frequency histograms depends on the number of individuals captured. This is why we will be using multiple gear types to find the most effective way to capture stonecats. Another limitation is experience bias. This is a concern with both gear use, and ageing otoliths. 9 Measurement Velocity (m/s) Min 0 0 0.25 Max 0.68 0.38 1.54 0.03 0.05 0.46 0.42 Avg 0.071 0.72 n 28 46 344 Location Big Penny MO Casselman River MD Assiniboine CAN Sources Banks and Distefano 2002 Kline and Morgan 2000 McCulloch and Franzin 1996 Depth (m) 29 Big Penny MO Banks and Distefano 2002 0.2 46 Casselman River MD Kline and Morgan 2000 0.4 1 Lyon Creek KA Layer and Wood 19866 0.15 1.2 0.5 344 Assiniboine CAN McCulloch and Franzin 1996 0.45 0.45 0.45 274 Little Saskatchewan CAN McCulloch and Franzin 1996 0.8 1 Several Tributaries to Assiniboine CAN McCulloch and Franzin 1996 0.25 1.17 0.87 Meramec River MO Walsh and Burr 1985 Table1. A summary of velocity and depths where stonecats have been observed including, when available; minimum (min) maximum (max) and average (avg) velocity or depth at each location, total number of individuals observed (n), river of each observation and state or country (Canada), and source. Boulder >250mm Cobble 40200mm Pebble 1564mm Gravel 2-16mm Sand <2mm Detritus n Location Sources 0-.23 .03-.52 >.4 0.61 0.1 0.67* 0.86* .07-.91 >.4 0.35 0.3 .02-.33 0-.15 0-.47 Big Penny MO Mas de Cyhgnes MO Casselman River MD Lyon Creek KA Assiniboine CAN Little Saskatchewan CAN Several Tributaries to Assiniboine Banks and Distefano 2002 Brewer et al. 2006 Kline and Morgan 2000 Layer and Wood 1986 McCulloch and Franzin 1996 McCulloch and Franzin 1996 0.02 0.3 0.00 0.75* 1.00* 0.08* 0.64* 0.1 0.55* 0.00* 29 140 46 1 344 274 1.00* 0.00* 1.00* 1 0.02 McCulloch and Franzin 1996 Table 2. A summary of percent substrate where stonecats have been observed, using a modified Wentworth scale noting the size class, total number of individuals observed (n), river of each observation and state or country (Canada), and source. *denotes that the particle size classes where not reported in the paper and was therefore assumed. 10 Source Gilbert 1953 Ohio Streams Walsh and Burr 1985 IL and MO rivers Average (mm) n Average (mm) n Age0+ 53.6 47 Age1+ 72.6 34 Age2+ 89.0 29 48.6 1 Age3+ 104.1 23 Age4+ 116.4 16 Age5+ 128.9 10 100 17 123.3 7 177 2 Table 3. A summary of the average lengths in millimeters of stonecats for each age class with the number of individuals (n) sampled. Figure 1. Known distribution of stonecat (Page and Burr 2006). Figure 2. An example of a substrate type GIS layer from the humminbird (Kaeser and Litts 2010) 11 References Anderson, R. O., and R. M. Neumann. 1996. Length, weight, and associated structural indices. Pages 447-482 in B. R. Murphy, and D. W. 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