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Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound Potentially Harmful Activity (X) Bottom trawl Fishing Scallop dredges Clam dredges Midwater trawl Gillnets (groundfish) Gillnets (pelagic) Long line Scottish seining Purse seining Recreational cod fishery Crab pots Lobster pots Whelk pots Otter trapping Other Seal hunt harvest Seabird hunt Seaweed harvest Anchor drops/drags Seabed Ore spill alteration Fish offal dumping Finfish aquaculture Dredge spoil dumping Dredging Mining Cables Freshwater diversion Subtidal construction Coastal Intertidal/coastal alteration construction Other (specify) Vessel traffic Disturbance Ship strikes Ecotourism Marine construction Seismic surveys Navy sonar Other (specify) X X Potentially Harmful Stressor (X) Oil pollution Industrial effluent Marine Fishplant effluent pollution Sewage Historic military waste Long range transport of nutrients Acid rain Persistent Organic Pollutants (POPs) Eutrophication Ghost nets Litter Other contaminants (specify) Ice distribution Climate Temperature change Change Sea-level rise Ocean acidification Current shifts Increased storm events Increased UV light Oxygen depletion Changes in freshwater runoff Other (specify) Green crab Harmful Membranipora species Golden Star Tunicate Violet Tunicate Vase Tunicate Codium fragile Clubbed Tunicate Didemnum Toxic Algal Blooms Disease organisms (human waste) Disease organisms (aquaculture) Other harmful species (specify) Other X X X X X 1 Gillnets (bottom): Fishing mortality is considered the greatest threat to Smith Sound cod, and there is a risk that fishing inshore may impede recovery of the entire stock (Fisheries and Oceans Canada, 2008). Following the discovery of dense aggregations of cod in Smith Sound in 1995, a small (index) fishery directed at these inshore populations was introduced in 1998. Catch rates declined and the fishery was closed in 2003. Catches during 2004-2005 were limited mainly to bycatch (>600t) in the winter flounder fishery (Fisheries and Oceans Canada, 2008) and sentinel fisheries. Sentinel catch rates near Trinity Bay (southern 3K and northern 3L) have generally increased since 2002 and are currently above average for the time series. A directed stewardship fishery was reopened in the inshore in 2006 to replace the index fishery in 2006. Reported landings from the 2007 stewardship fishery were 2364t. In addition, 182t were landed in the sentinel fishery. These fisheries largely utilize gillnets. Bycatch in other directed fisheries, including winter flounder and lumpfish, which utilize gillnets, are also significant. Total fishing mortality is estimated at 20% of the biomass (Corey Morris, Biologist, Fisheries and Oceans Canada, PO Box 5667, St. John’s, NL, A1C 5X1, “pers. comm.”). Stewardship fishery catch rates in 2006-07 were slightly higher than in earlier fisheries between 1998 and 2002. A pre-recruit index suggests that the strength of the 2003-2006 year-classes will be much lower than those that have supported recent fisheries (Fisheries and Oceans Canada, 2008). Gillnet fishing is clearly a major source of mortality and has been screened in for further analysis. Screened in. Recreational cod fishery: Historically, cod has been an important part of the diet in Newfoundland, and access to a winter supply of fish is considered a traditional right which residents took for granted until the implementation of the groundfish moratorium. As a result, there was intense pressure to open a food/recreational fishery when dense aggregations of fish were detected in Smith Sound and adjacent coastal areas in 1995. In response to public pressure, a food fishery was opened for a number of years, but was closed again in 2003 in response to declining inshore stocks. The fishery was reopened in 2006. Only handline and angling gear is permitted. Handlines include baited hooks, feathered hooks and artificial lures. A maximum of three (3) hooks per line may be used. The season dates are set each year, typically 3-4 weeks in late July/early August, and an additional 1-2 weeks in late September/early October, for a total of five weeks. Recreational fishers are limited to five (5) groundfish per day (including cod), and 15 per boat trip. Estimates of landings from the recreational fishery are variable. The 2007 DFO Survey (BriLev Consulting Inc., 2008) estimated that anglers caught 1,128,635 fish in the 2007 recreational fishery, with 308,160 in Trinity Bay alone. This suggests that the recreational catch was equivalent to that of the stewardship fishery (Fisheries and Oceans Canada, 2008), and may be a significant stressor to Smith Sound cod. Screened in. Ghost nets: Ghost nets are fishing gear that have been lost or discarded at sea. Fishing, legal or otherwise, involves an inherent risk of gear loss. Factors such as weather, currents, tides, sea 2 state, depth, fishing intensity, presence of sea ice, the make up of the seafloor, the condition of the gear, equipment and vessel all contribute to the risk of lost gear (Hareide, N-R. et al., 2005; The British Ecological Society, 2000). Since the 1960s, fishing nets have been constructed from highly durable plastic materials such as nylon, polypropylene and polyethylene, which are largely impervious to biodegradation- they are resistant to chemicals and abrasion (National Academy of Sciences, 2008). Unlike their natural predecessors, the new materials can last for years or decades in the marine environment, and lost gear or even torn fragments of netting or line floating in the sea, can continue to fish for considerable periods (The British Ecological Society, 2000). Lost gillnets, traps, trawls and line fisheries are considered the most harmful (National Academy of Sciences, 2008), and of those, gillnets are generally thought to be the most problematic. Set bottom gillnets, by virtue of their fixed, anchored framing, may remain fully deployed and fishing long after they are lost or abandoned. As nets become fouled, they become more visible, lose their vertical profile and their fishing capacity declines, but limited investigations have shown that gillnets lost in deepwater (>400m) can fish for years after they are lost because there is very little bio-fouling or water movement in depths below 400m (National Academy of Sciences, 2008). Even when nets collapse, forming balls on the sea floor, they continue to fish. Recent studies of nets on the seabed have shown that a typical pattern of capture is observed. Over the first few days, catches decline almost exponentially as the increasing weight of the catch causes the net to collapse. Then for the next few weeks, the decay of captured animals attracts a large number of scavenger species such as crabs, lobster and fish. This cycle of capture, decay and attraction continues for as long as the net retains entanglement properties. Once on the bottom, monofilament nets may, once clear of fish remains, disentangle, return to an upright position and resume fishing (The British Ecological Society, 2000). We have no data on the number of ghost nets in Smith Sound, but data from other areas indicates that the problem is likely to be significant. The Northwest Straits Commission estimates that there are nearly 3,900 gillnet remaining in Puget Sound from domestic salmon fisheries from the 1970s and 1980s. In a recent survey of over 1,000 fish harvesters currently operating within Placentia Bay, 67% reported experiencing loss of gear (FFAW, 2007), and both DFO and industry recognized it as a major concern for Atlantic Canadian fish harvesters. A ghost net retrieval program conducted in Placentia Bay in the 1990s retrieved sixty ghost nets containing 30,000 lbs of rotting cod, as well as other species. Some 10,000 vessels, mainly small boat, inshore operations, fished monofilament gillnets in Atlantic Canada prior to the northern cod moratorium. While it is difficult to quantify the amount of lost gear, studies suggest that some 8,000 active gillnets were lost on average each year for a number of years up to 1992. In a survey of 100 Atlantic Canada gillnet fish harvesters, losses averaged 1-3 nets per fisher per year, with the exception of two fishers with vessels greater than 65 feet that incurred an average loss of 19.2 nets per year (Memorial University of Newfoundland & Fisheries and Oceans Canada, 1995). 3 Gillnets are considered the most problematic gear in relation to fish mortality, and are the most common gear used in Smith Sound. Smith Sound is a small, narrow, relatively sheltered area where significant gear loss is unlikely to occur, but any lost gear is likely to end up in one of the two deep trenches where dense aggregations of cod overwinter, and significant mortalities could result. Screened in. Temperature change: Drinkwater (UNEP & UNFCCC, 2002) predicts a temperature increase of 2-4oC in Southern Newfoundland waters by 2100 based on IPCC 2001 models. Temperature rise will likely not be linear, but is expected to accelerate over time. Even given the worst case scenario, an increase in 0.4oC is likely the most we can expect over the next ten years. Many believe that temperature shifts were at least partially responsible for the poor recovery of over-fished cod stocks in the 1990s (Rose, G. A., 2007). Drinkwater states that the range of cod may extend northward with increasing temperature, and it is likely that spring migrations will occur earlier, and fall returns will be later (Drinkwater, K. F., 2005). These responses of cod to future climate changes are highly uncertain, however, as they will also depend on the changes to climate and oceanographic variables besides temperature, such as stratification, plankton production, the prey and predator dynamics, and industrial fishing. Temperature changes are not likely to be significant over the next 10 years, and a small increase of 0.4oC or less would likely be beneficial to cod in Smith Sound. Screened out. Increased storm events: Recent scientific evidence suggests a link between the destructive power, or intensity, of hurricanes and higher ocean temperatures, driven in large part by global warming. Two factors that contribute to more intense tropical cyclones, ocean heat content and atmospheric water vapour, have both increased over the past several decades. As warm, moist air rises, it lowers air pressure at sea level and draws the surrounding air inward and upward in a rotating pattern, powering the storm. As the moist air spirals in and rises to higher altitudes, it cools and releases heat as it condenses to rain (Union of Concerned Scientists, 2006). Atlantic tropical cyclones are getting stronger on average, with a 30-year trend that has been related to an increase in ocean temperatures, and are predicted to impact the NW Atlantic at a high level of intensity relative to other areas of the globe (Elsner, J. B., Kossin, J. P., & Jagger, T. H., 2008). The years 1995-2000 experienced the highest level of North Atlantic hurricane activity in the reliable record (Goldenberg, S. B., Landsea, C. W., Mestas-Nunez, A. M., & Gray, W. M., 2001). The largest increase in hurricanes reaching categories 4 and 5 occurred in the Pacific and Indian Oceans, but the highest increase in the number of cyclones and cyclone days occurred in the North Atlantic (Webster, P. J, Holland, G. J., Curry, J. A., & Chang, H. A., 2005). The relationships between a warming environment and increasing storm events is complex, and research results and predictions are variable, and more research is clearly required (Emanuel, K., 2005; Emanuel, K. A., 2000; Goldenberg, S. B., Landsea, C. W., Mestas-Nunez, A. M., & Gray, W. M., 2001; Webster, P. J, Holland, G. J., Curry, J. A., & Chang, H. A., 2005). Increased storm surges can potentially contribute to super-cooling events during severe winter storms where the motion keeps seawater in a liquid state at temperatures well below - 4 2oC and can lead to mass mortalities. A super-cooling event in Smith Sound several winters ago resulted in mass mortality (~500,000 fish) of overwintering cod. Screened in. Green crab (Carcinus maenas): The European green crab is an aggressive and hardy invasive species that has significant impact on eelgrass beds as a result of their burrowing activity, which has been well documented in PEI, as well as North Harbour, Placentia Bay. Smith Sound has extensive eelgrass beds in the shallow inner portion of the Sound, and since eelgrass is considered an important nursery habitat for juvenile cod, green crab may potentially impact cod nursery habitat in Smith Sound. Green crab was first detected in North Harbour, Placentia Bay in 2007, and has since been found in several sites in Placentia Bay as well as two sites on the west coast. Green crab have not been detected in Trinity Bay, but since this invasive species was first detected in North Harbour, Placentia Bay, it has expanded rapidly within Placentia Bay in two years and was recently identified near Port aux Basques, and in the Bay St. George region. Northern waters of the LOMA may be protected by colder water temperatures, but green crab is unlikely to reach high concentrations in Trinity Bay in the near future. Screened out. 5 Lacey bryozoan (Membranipora membranacea): Membranipora is an invasive species which was first detected by MUN Scientist Bob Hooper in Bonne Bay in 2002, and has since spread to many coastal areas of the LOMA. The map below shows survey areas where Membranipora has been detected: This invasive colonial bryozoan of European origin grows on kelp, rockweed, eelgrass and other marine plants, secreting a protective limestone covering which forms a tough, white lace-like crust over the flexible, rubbery surface of the kelp blade. Kelp blades that are heavily encrusted with Membranipora become brittle and more susceptible to breakage during a storm surge. In high energy areas, encrusted blades are far more prone to break off. In some areas this has led to the removal of entire kelp beds. Membranipora is expected to have a significant impact on the structural habitat provided by kelp and to a lesser degree rockweed, with implications for biodiversity and recruitment of juvenile fish such as cod which utilize kelp beds as nursery habitat. Mature kelp beds are being killed on the north coast of Newfoundland, while young and mature kelp are affected on the south coast of the island. Water temperature is critical for the growth of Membranipora with maximum growth at water temperatures reaching 15oC, usually in August in most areas, with growth continuing until December. The impact on the kelp peaks in November. Kelp on the west and south coasts have suffered major impacts as a result of this AIS, with kelp basically going from a perennial to annual. On the Northeast coast, Membranipora is present but the level of harm to kelp is much lower. Climate change could potentially intensify the growth of this harmful species, but significant impacts on kelp are not expected in Smith Sound over the next ten years. Screened out. Key Activities/Stressors: Gillnets (bottom) Recreational cod fishery Ghost nets Increased storm events 6 Reference List 1. BriLev Consulting Inc. (2008). 2007 Survey of the Recreational Cod fishery of Newfoundland and Labrador. 2. Drinkwater, K. F. (2005). The response of Atlantic cod (Gadus morhua) to future climate change. ICES Journal of Marine Science, 62, 1327-1337. 3. Elsner, J. B., Kossin, J. P., & Jagger, T. H. (2008). The increasing intensity of the strongest tropical cyclones. Nature, 455, 92-95. 4. Emanuel, K. (2005). Increasing Destructiveness of Tropical Cyclones over the past 30 Years. Nature, 436, 686-688. 5. Emanuel, K. A. (2000). A Statistical Analysis of Tropical Cyclone Intensity. Mon.Wea.Rev., 128, 1139-1152. 6. FFAW (2007). Appendix C: Co-existence? Fishing Activity and Tanker Traffic in Placentia Bay, June 2007 (Rep. No. Provincial Environmental Assessment, Environmental Impact Statement, Volume 4, Socio-Economic Assessment, Volume 2). Newfoundland and Labrador Refining Corporation. 7. Fisheries and Oceans Canada (2008). Stock Assessment of Northern (2J3KL) Cod in 2008 (Rep. No. 2008/034). Canadian Science Advisory Secretariat Science Advisory Report, Newfoundland and Labrador Region. 8. Goldenberg, S. B., Landsea, C. W., Mestas-Nunez, A. M., & Gray, W. M. (2001). The Recent Increase in Atlantic Hurricane Activity: Causes and Implications. Science, 293, 474-479. 9. Hareide, N.-R., Garnes, G., Rihan, D., Mulligan, M., Tyndall, P., Clark, M., Connolly, P., Misund, R., McMullen, P., Furevik, D., Humborstad, O. B., Høydal, K., & Blasdale, T. (2005). A preliminary Investigation on Shelf Edge and Deepwater Fixed Net Fisheries to the West and North of Great Britain, Ireland, around Rockall and Hatton Bank. 10. Memorial University of Newfoundland & Fisheries and Oceans Canada (1995). Phase I: Prevention of ghost fishing in Atlantic Canada. Fisheries and Marine Institute of Memorial University of Newfoundland in cooperation with Fisheries Management, Fisheries and Oceans Canada. 11. National Academy of Sciences (2008). Tackling Marine Debris in the 21st Century. 12. Rose, G. A. (2007). Cod: The Ecological History of the North Atlantic Fisheries. Breakwater Books. 7 13. The British Ecological Society. Commercial fishing: the wider ecological impacts. Moore, G. and Jennings, S. Ecological Issues , 1-66. 2000. Ref Type: Serial (Book,Monograph) 14. UNEP & UNFCCC (2002). Climate Change Information Kit UNEP and UNFCCC. 15. Union of Concerned Scientists (2006). Hurricanes and Climate Change: Exploring the potential causes of increased storm intensity. Union of Concerned Scientists, Global Warming. [Announcement posted on the World Wide Web]. from the World Wide Web: http://www.ucsusa.org/global_warming/science_and_impacts/science/hurrican es-and-climate-change.html 16. Webster, P. J., Holland, G. J., Curry, J. A., & Chang, H. A. (2005). Changes in Tropical Cyclone Number, Duration, and Intensity in a Warming Environment. Science, 309, 1844-1846. 8 Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound Gillnets (bottom) Magnitude of Interaction Areal extent: Smith Sound is a small area which provides refuge for dense aggregations of mature cod throughout the winter and spring. A deep (200m) trench provides over-wintering habitat for pre-spawning fish, and as deep waters cool in the spring, warming surface layers provide above zero waters if deep water should fall below optimal temperatures for spawning and survival of cod. During the spawning season (April-July), cod may be seen throughout Smith Sound. Some fish appear to remain in Smith Sound all year, but the majority migrate seasonally in and out of the bay. Tagging studies indicate that migrating cod begin to move out of the sound in April, into coastal waters and bays both north and south of Trinity Bay, with some larger fish moving offshore (Corey Morris, Biologist, Fisheries and Oceans Canada, PO Box 5667, St. John’s, NL, A1C 5X1, “pers. comm.”). In a normal year, migrating cod return to Smith Sound in late fall or early winter when deep waters in the trench are warm (3-5oC) (Rose, 2007). Extensive eelgrass beds at the head of the Sound and kelp beds within the Sound provide nursery habitat for juvenile fish. Figure 1. Cod distributions in Trinity Bay from acoustic surveys (O'Driscoll et al., 2000) Gillnet fishing within Smith Sound may include directed sentinel and stewardship fisheries, and winter flounder and lumpfish fisheries. There are no restrictions on the locations of these fisheries within the Sound, therefore, we have assumed that the entire EBSA is subject to gillnet fishing. Score 10 Contact: In relation to bottom gillnet, Quantitative Fishing Gear Scores (Fisheries and Oceans Canada, 2007) for “contact” are high (75-100%) for bony fish species. Since there is a directed fishery for cod in Trinity Bay and adjacent waters where migrating cod from Smith Sound may occur, we have given a score of 100%. A component of the CP is nursery habitat which is not affected by gillnet fisheries, so the score has been reduced by 25%. Score 7.5 Duration: Cod occur in Smith Sound throughout the year, but aggregations are greatest from November through April. The main directed fisheries for cod using bottom gillnet occur in the late summer or fall (September- October), including the stewardship and sentinel fisheries. Bycatch of cod may occur in other gillnet fisheries including the winter flounder fishery (August), and the turbot and lumpfish fisheries which typically takes place in June-July. The turbot fishery does not take place within the bay, but may impact migrating cod. June-October = 5months/12months = 42%. Score 4.2 Intensity: Halpern et al. (2008) have developed maps showing the global intensity of several anthropogenic stressors including ‘demersal non-destructive fishing with high bycatch’, which includes bottom gillnet fisheries (see Figure below). This map can be used to provide guidance in scoring the intensity of a stressor in relation to maximum intensity in a global context, in accordance with the scale provided below. This map shows a medium (yellow) intensity relative to global levels for a score range of 40% to 60% for the LOMA. Map colour Red Orange Yellow Light Blue Dark Blue Intensity 80-100% 60-80% 40-60% 20-40% 0-20% Figure 2. Global intensity of bottom gillnets, adapted from (Halpern et al., 2008). Gillnets are the dominant gear impacting cod within the inshore, with landings of cod (including bycatch) estimated at 2500t in 2007. Although landings are greatly reduced compared to historical levels, landings are significant in relation to the estimated biomass of inshore stocks (10%). Fishing intensity is minimal during the spawning period (AprilJuly). We have therefore selected the lowest score within the range. Score 4 Magnitude of Interaction: (10 x 7.5 x 4.2 x 4)/1000 = 1.3 Sensitivity Sensitivity of the CP to acute impacts: In relation to bottom gillnet, Quantitative Fishing Gear Scores (Fisheries and Oceans Canada, 2007) for “harm” are high (75-100%) for bony fish species in 3NO. Bottom gillnets were also given a “high impact” rating in relation to groundfish based on ecological impact (Fuller et al., 2008). Directed fisheries (sentinel and stewardship) which predominantly use bottom gillnets are responsible for significant mortality (up to10% of biomass) of inshore cod which utilize Smith Sound at some stage in their life cycle for spawning, refuge, nursery and/or migration. Since there is a directed gillnet fishery targeting cod, we have selected a moderate score in the high range – score 9. Since juvenile (nursery) fish are not directly targeted by gillnet the score has been reduced by 25%. Score 6.8 Sensitivity of the CP to chronic impacts: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod which was assessed by COSEWIC in 2003 and designated endangered. The Status Report lists fishing (including legal, illegal, and unreported catches) and fishing-induced changes to the ecosystem as key threats to cod recovery. Inshore components of the stock appear more productive than offshore components. Stewardship fishery catch rates in 2006-07 were slightly higher than in earlier fisheries between 1998 and 2002, and sentinel fisheries catch rates near Trinity Bay (southern 3K and northern 3L) have generally increased since 2002 and are currently above average for the time series. A pre-recruit index suggests that the strength of the 2003-2006 year-classes will be much lower than those that have supported recent fisheries (Fisheries and Oceans Canada, 2008). Clearly, significant fishing mortality can affect the long-term stability of the stock, and therefore we have selected a moderate score (5). Atlantic cod are listed in the CP document as a ‘depleted and rare species’, and will therefore rank higher on this scale than other CPs because they are already in need of recovery (add one point). Score 6 Sensitivity of ecosystem to harmful impacts to the CP: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod, one of two major cod stocks within the LOMA. Cod have historically had a huge influence on the ecosystem of the LOMA, mainly because of their large biomass and broad distribution compared to other species, and their significant role as both predator and prey at all trophic levels as they grow and move from one trophic level to another. Even though they are currently at less then one percent of their former biomass, they still represent a significant component of the total goundfish population. Since the sharp decline in cod biomass in the 1990s, stocks of invertebrates such as shrimp and crab have expanded to record highs in what has been termed a trophic cascade. These changes have been blamed on over-fishing resulting in perturbations to the predator-prey systems, and although environmental change may have had a contribution, it is clear that the role of Atlantic cod in the ecosystem is highly significant to its structure and function. Coastal bays provide significant spawning, nursery and over-wintering habitat for Atlantic cod within the LOMA. Since the collapse of the cod stocks in the early 1990s, much of the remaining biomass has been concentrated in coastal regions. Although cod were historically known to over-winter and spawn in these coastal areas, the recent concentration of cod in coastal bays, in contrast to the dearth of fish in adjacent shelf regions, may be without precedent (Lawson & Rose, 2000). Bay stocks are seen by many as a key component in the recovery of cod stocks within the LOMA as a whole. Smith Sound is an important overwintering area for the severely depleted population of Northern cod. The very dense aggregation of fish in the relatively small geographical area of Smith Sound during the winter not only represents the largest group in terms of numbers of fish, but the fish are also very large in size and hence very fecund, and can potentially contribute significant numbers of eggs to Smith Sound and adjacent areas. Smith Sound is considered the largest remaining spawning area for Northern Cod. Extensive eelgrass beds at the head of the Sound provide high quality nursery habitat. Much of the currently known spawning that occurs along the northeast coast appears to originate from migrating subgroups of cod which overwintered in Smith Sound (Templeman, 2007). Smith Sound cod aggregations may be critical to the recovery of the population (Templeman, 2007), although the potential role of bay stocks such as those in Smith Sound in rebuilding the offshore stocks is unknown (Rose, 2007). Given the importance of this population to one of the two major stocks within the LOMA, we have selected a score of 6. Atlantic cod are listed in the CP document as an ‘ecologically significant species’ (add one point). Score 7 Sensitivity: (6.8 + 6 + 7)/3 = 6.6 Risk of Harm: MoI x S = 1.3 x 6.6 = 8.6 Certainty Checklist Answer yes or no to all of the following questions. Record the number of NO’s to the 9 questions, and record certainty according to the scale provided below: 1 No’s = High certainty 2- 3 No’s = Medium certainty >4 No’s = Low certainty Y/N N Is the score supported by a large body of information? Y Is the score supported by general expert agreement? Y Is the interaction well understood, without major information gaps/sources of error? Y Is the current level of understanding based on empirical data rather than models, anecdotal information or probable scenarios? N Is the score supported by data which is specific to the region, (EBSA, LOMA, NW Atlantic? Y Is the score supported by recent data or research (the last 10 years or less)? Y Is the score supported by long-term data sets (ten years or more) from multiple surveys (5 years or more)? Y Do you have a reasonable level of comfort in the scoring/conclusions? N Do you have a high level of confidence in the scoring/conclusions? Certainty Score: Medium Reference List 1. Fisheries and Oceans Canada (2007). Draft proceedings of the Workshop on Qualitative Risk Assessment of Fishing Gears. In Government of Canada. 2. Fisheries and Oceans Canada (2008). Stock Assessment of Northern (2J3KL) Cod in 2008 (Rep. No. 2008/034). Canadian Science Advisory Secretariat Science Advisory Report, Newfoundland and Labrador Region. 3. Fuller, S. D., Picco, C., Ford, J., Tsao, C.-F., Morgan, L. E., Hangaard, D. et al. (2008). How we fish matters: Addressing the Ecological Impacts of Canadian Fishing Gear Ecology Action Centre, Living Oceans Society, and Marine Conservation Biology Institute. 4. Halpern, B. S., Walbridge, S., Selkoe, K. A., Kappel, C. V., Micheli, F., D'Agrosa, C. et al. (2008). A Global Map of Human Impact on Marine Ecosystems. Science, 319, 948-952. 5. Lawson, G. L. & Rose, G. A. (2000). Seasonal distribution and movements of coastal cod (Gadus morhua L.) in Placentia Bay, Newfoundland. Fisheries Research, 49, 6175. 6. O'Driscoll, R. L., Rose, G. A., Andersdon, J. T., & Mowbray, F. (2000). Spatial association between cod and capelin: a perspective on the inshore-offshore dichotomy (Rep. No. 2000/083). 7. Rose, G. A. (2007). Cod: The Ecological History of the North Atlantic Fisheries. Breakwater Books. 8. Templeman, N. D. (2007). Placentia Bay-Grand Banks Large Ocean Management Area Ecologically and Biologically Significant Areas (Rep. No. 2007/052). Canadian Science Advisory Secretariat Research Document, Fisheries and Oceans Canada. Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound Recreational cod fishery Magnitude of Interaction Areal extent: Smith Sound is a small area which provides refuge for dense aggregations of mature cod throughout the winter and spring. A deep (200m) trench provides over-wintering habitat for pre-spawning fish, and as deep waters cool in the spring, warming surface layers provide above zero waters if deep water should fall below optimal temperatures for spawning and survival of cod. During the spawning season (April-July), cod may be seen throughout Smith Sound. Some fish appear to remain in Smith Sound all year, but the majority migrate seasonally in and out of the bay. Tagging studies indicate that migrating cod begin to move out of the Sound in April, into coastal waters and bays both north and south of Trinity Bay, with some larger fish moving offshore (Corey Morris, Biologist, Fisheries and Oceans Canada, PO Box 5667, St. John’s, NL, A1C 5X1, “pers. comm.”). In a normal year, migrating cod return to Smith Sound in late fall or early winter when deep waters in the trench are warm (3-5oC) (Rose, 2007). Extensive eelgrass beds at the head of the Sound and kelp beds within the Sound provide nursery habitat for juvenile fish. Figure 1. Cod distributions in Trinity Bay from acoustic surveys (O'Driscoll et al., 2000) The recreational cod fishery occurs throughout Smith Sound wherever cod are found. Score 10 Contact: Since there is a directed recreational fishery for cod in Trinity Bay, we have given a score of 100%. A component of the CP is cod nursing (juvenile fish) which is not affected by the recreational cod fishery, so the score has been reduced by 25%. Score 7.5 Duration: The cod are widely distributed in Smith Sound throughout the year. The recreational cod fishery is conducted in the fall, although dates are variable. The 2007 fishery was open for five weeks (35 days): July 25 to August 19 and September 29 to October 7. 35 days/365 days = 9.5% Score 1 Intensity: Halpern et al. (2008) have developed maps showing the global intensity of several anthropogenic stressors including ‘demersal non-destructive fishing with low bycatch’, which includes handline fisheries (see Figure below). This map can be used to provide guidance in scoring the intensity of a stressor in relation to maximum intensity in a global context, in accordance with the scale provided below. This map shows a medium-low (light blue) intensity for the EBSA and other coastal areas of the LOMA relative to global levels, for a score range of 20% to 40%. Map colour Intensity Red 80-100% Orange 60-80% Yellow 40-60% Light Blue 20-40% Dark Blue 0-20% Figure 2. Global intensity of handline fisheries, adapted from (Halpern et al., 2008). Landings of cod in Trinity Bay by the recreational cod fishery were the highest of any area in the region, amounting to 308,160 fish in 2007, almost 40% of the total landings within the LOMA. These landings are significant (equivalent to that of the commercial fishery), and were particularly high in Trinity Bay compared to other areas of the LOMA, so we have selected highest score in the global range (20-40%). Score 4 Magnitude of Interaction: (10 x 7.5 x 1 x 4)/1000 = 0.3 Sensitivity Sensitivity of the CP to acute impacts: Since there is a directed recreational fishery for cod in Trinity Bay, we have given a score in the high range. Landings of cod in Trinity Bay by the recreational cod fishery were the highest of any area in the region, amounting to 308,160 fish in 2007, almost 40% of the total landings within the LOMA. These landings are significant (equivalent to that of the commercial fishery), and were particularly high in Trinity Bay compared to other areas of the LOMA, so we have selected highest score in the high range (Fisheries and Ocean Canada, 2007). A component of the CP is nursery habitat which is not affected by the recreational cod fishery, so the score has been reduced by 25%. Score 7.5 Sensitivity of the CP to chronic impacts: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod which was assessed by COSEWIC in 2003 and designated endangered. The Status Report lists fishing (including legal, illegal and unreported catches) and fishing-induced changes to the ecosystem as key threats to cod recovery. Inshore components of the stock appear more productive than offshore components. Stewardship fishery catch rates in 2006-07 were slightly higher than in earlier fisheries between 1998 and 2002, and sentinel fisheries catch rates near Trinity Bay (southern 3K and northern 3L) have generally increased since 2002 and are currently above average for the time series. A pre-recruit index suggests that the strength of the 2003-2006 year-classes will be much lower than those that have supported recent fisheries (Fisheries and Oceans Canada, 2008). Fishing mortality associated with the recreational fishery was particularly high in Smith Sound, although not extreme, and this level of fishing may affect the long term stability of the stock so we have selected a score at the low end of the high range (7.5). Atlantic cod are listed in the CP document as a ‘depleted and rare species’, and will therefore rank higher on this scale than other CPs because they are already in need of recovery (add one point). Score 8.5 Sensitivity of the ecosystem to harmful impacts to the CP: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod, one of two major cod stocks within the LOMA. Cod have historically had a huge influence on the ecosystem of the LOMA, mainly because of their large biomass and broad distribution compared to other species, and their significant role as both predator and prey at all trophic levels as they grow and move from one trophic level to another. Even though they are currently at less then one percent of their former biomass, they still represent a significant component of the total goundfish population. Since the sharp decline in cod biomass in the 1990s, stocks of invertebrates such as shrimp and crab have expanded to record highs in what has been termed a trophic cascade. These changes have been blamed on over-fishing resulting in perturbations to the predator-prey systems, and although environmental change may have had a contribution, it is clear that the role of Atlantic cod in the ecosystem is highly significant to its structure and function. Coastal bays provide significant spawning, nursery and over-wintering habitat for Atlantic cod within the LOMA. Since the collapse of the cod stocks in the early 1990s, much of the remaining biomass has been concentrated in coastal regions. Although cod were historically known to over-winter and spawn in these coastal areas, the recent concentration of cod in coastal bays, in contrast to the dearth of fish in adjacent shelf regions, may be without precedent (Lawson & Rose, 2000). Bay stocks are seen by many as a key component in the recovery of cod stocks within the LOMA as a whole. Smith Sound is an important overwintering area for the severely depleted population of Northern cod. The very dense aggregation of fish in the relatively small geographical area of Smith Sound during the winter not only represents the largest group in terms of numbers of fish, but the fish are also very large in size and hence fecundity, and can potentially contribute significant numbers of eggs to Smith Sound and adjacent areas. Smith Sound is considered the largest remaining spawning area for Northern Cod. Extensive eelgrass beds at the head of the Sound provide high quality nursery habitat. Much of the currently known spawning that occurs along the northeast coast appears to originate from migrating subgroups of cod which overwintered in Smith Sound (Templeman, 2007). Smith Sound cod aggregations may be critical to the recovery of the population (Templeman, 2007), although the potential role of bay stocks such as those in Smith Sound in rebuilding the offshore stocks is unknown (Rose, 2007). Given the importance of this population to one of the two major stocks within the LOMA, we have selected a score of 6. Atlantic cod are listed in the CP document as an ‘ecologically significant species’ (add one point). Score 7 Sensitivity: (7.5 + 8.5 + 7)/3 = 7.7 Risk of Harm: MoI x S = 0.3 x 7.7 = 2.3 Certainty Checklist Answer yes or no to all of the following questions. Record the number of NO’s to the 9 questions, and record certainty according to the scale provided below: 1 No’s = High certainty 2- 3 No’s = Medium certainty No’s = Low certainty >4 Y/N N Is the score supported by a large body of information? Y Is the score supported by general expert agreement? Y Is the interaction well understood, without major information gaps/sources of error? Y Is the current level of understanding based on empirical data rather than models, anecdotal information or probable scenarios? N Is the score supported by data which is specific to the region, (EBSA, LOMA, NW Atlantic? Y Is the score supported by recent data or research (the last 10 years or less)? Y Is the score supported by long-term data sets (ten years or more) from multiple surveys (5 years or more)? Y Do you have a reasonable level of comfort in the scoring/conclusions? N Do you have a high level of confidence in the scoring/conclusions? Certainty Score: Medium For interactions with Low certainty, underline the main factor(s) contributing to the uncertainty Lack of comprehensive data Lack of expert agreement Predictions based of future scenarios which are difficult to predict Other (provide explanation) Suggest possible research to address uncertainty: Improved monitoring of recreational fishery Reference List 1. Fisheries and Ocean Canada (2007). Conservation Harvesting Plan (CHP), Atlanticwide for Mobile Gear Vessels 65-100', February 8, 2007 (unpublished) Fisheries and Oceans Canada, Newfoundland & Labrador Region. 2. Fisheries and Oceans Canada (2008). Stock Assessment of Northern (2J3KL) Cod in 2008 (Rep. No. 2008/034). Canadian Science Advisory Secretariat Science Advisory Report, Newfoundland and Labrador Region. 3. Halpern, B. S., Walbridge, S., Selkoe, K. A., Kappel, C. V., Micheli, F., D'Agrosa, C. et al. (2008). A Global Map of Human Impact on Marine Ecosystems. Science, 319, 948-952. 4. Lawson, G. L. & Rose, G. A. (2000). Seasonal distribution and movements of coastal cod (Gadus morhua L.) in Placentia Bay, Newfoundland. Fisheries Research, 49, 6175. 5. O'Driscoll, R. L., Rose, G. A., Andersdon, J. T., & Mowbray, F. (2000). Spatial association between cod and capelin: a perspective on the inshore-offshore dichotomy (Rep. No. 2000/083). 6. Rose, G. A. (2007). Cod: The Ecological History of the North Atlantic Fisheries. Breakwater Books. 7. Templeman, N. D. (2007). Placentia Bay-Grand Banks Large Ocean Management Area Ecologically and Biologically Significant Areas (Rep. No. 2007/052). Canadian Science Advisory Secretariat Research Document, Fisheries and Oceans Canada. Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound Ghost nets (derelict fishing gear) Magnitude of Interaction Areal extent: Adult and juvenile cod are widely distributed throughout Smith Sound, depending on the season and the life stage. The approximate dimensions of Smith Sound are 37 km x 2.5 = 92.5 km2. As a result of the steep bathymetry, any lost nets are most likely to accumulate in the deep trenches where cod aggregate in winter. The approximate dimensions of the trenches are 11 km x 1 = 11 km2 (Corey Morris, Biologist, Fisheries and Oceans Canada, PO Box 5667, St. John’s, NL, A1C 5X1, “pers. comm.”). As a result, the area of overlap is likely in the low range (11/92.5 = 12%), with most of the nets located in ~12% of the Sound. We have selected a slightly high score since some nets may be distributed in other areas of the Sound. Score 1.5 Contact: Contact with adult cod, particularly overwintering and migrating cod is considered high (8). Contact with juvenile cod is low, and spawning cod in Smith Sound are often reported to be high in the water column where water is warmer in spring, and contact would low. Overall, contact is therefore considered to be in the medium range. Score 4 Duration: Since the 1960s, fishing nets have been constructed from highly durable plastic materials such as nylon, polypropylene and polyethylene, which do not biodegrade. When exposed to the sun for a period of years, photo-degradation will weaken these materials releasing fragments of plastic. On the sea bottom, however, where they are protected from UV radiation, there is no evidence that these nets weaken or degrade over time. As a result, lost nets accumulate in the environment, and are present 100% of the time. Score 10 Intensity: Since we have no data on the density of ghost nets or the frequency of gear loss within the EBSA, we have based our intensity scores on data related to sources of ghost nets (gillnet fishing) and environmental factors (rough bottom, wind speed, wave action). Halpern et al. (2008) have developed maps showing the global intensity of several anthropogenic stressors including ‘demersal non-destructive fishing with high bycatch’, which includes bottom gillnet fisheries (see Figure 2 below). This map can be used to 1 This map shows a medium (yellow) intensity relative to global levels for a score range of 40% to 60% for the LOMA. Map colour Intensity Red 80-100% Orange 60-80% Yellow 40-60% Light Blue 20-40% Dark Blue 0-20% Figure 2. Global intensity of bottom gillnets, adapted from (Halpern et al., 2008). Gillnets are among the most common gear types used inshore, and since Smith Sound is known for its dense aggregations of fish, intensity is likely higher than average. Based on these factors we have selected the highest score within the range indicated for the LOMA. Score 6 Magnitude of Interaction: (1.5 x 4 x 10 x 6)/1000 = 0.36 Sensitivity Sensitivity of the CP to acute impacts: Set gillnets, by virtue of their fixed, anchored framing (held in position by buoys on top and lead rope on bottom), may remain fully deployed and fishing long after they are lost or abandoned. As nets become fouled, they become more visible, lose their vertical profile and their fishing capacity declines (National Academy of Sciences, 2008). Even when nets collapse, forming balls on the sea floor, they have been observed to self bait such that predators and scavengers attracted to entangled animals are themselves entangled, thereby perpetuating the cycle of destruction. Based on available data, impacts are considered significant, but relative to fishing mortality are likely minor for a score of 3. Score 3 Sensitivity of the CP to chronic impacts: Although overall mortality of cod from ghost nets may be relatively minor in Smith Sound, the chronic, cumulative nature of the threat is a greater concern. Fishing activity can be reduced as required to conserve stocks, but once ghost nets are lost, retrieval is very difficult and expensive, and mortalities can continue for decades (minor, long term). 2 Atlantic cod are listed in the CP document as a ‘depleted and rare species’, and will therefore rank higher on this scale than other CPs because they are already in need of recovery (add one point). Score 3 Sensitivity of ecosystem to harmful impacts to the CP: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod, one of two major cod stocks within the LOMA. Cod have historically had a huge influence on the ecosystem of the LOMA, mainly because of their large biomass and broad distribution compared to other species, and their significant role as both predator and prey at all trophic levels as they grow and move from one trophic level to another. Even though they are currently at less then one percent of their former biomass, they still represent a significant component of the total goundfish population. Since the sharp decline in cod biomass in the 1990s, stocks of invertebrates such as shrimp and crab have expanded to record highs in what has been termed a trophic cascade. These changes have been blamed on over-fishing resulting in perturbations to the predator-prey systems, and although environmental change may have had a contribution, it is clear that the role of Atlantic cod in the ecosystem is highly significant to its structure and function. Coastal bays provide significant spawning, nursery and over-wintering habitat for Atlantic cod within the LOMA. Since the collapse of the cod stocks in the early 1990s, much of the remaining biomass has been concentrated in coastal regions. Although cod were historically known to over-winter and spawn in these coastal areas, the recent concentration of cod in coastal bays, in contrast to the dearth of fish in adjacent shelf regions, may be without precedent (Lawson & Rose, 2000). Bay stocks are seen by many as a key component in the recovery of cod stocks within the LOMA as a whole. Smith Sound is an important overwintering area for the severely depleted population of Northern cod. The very dense aggregation of fish in the relatively small geographical area of Smith Sound during the winter not only represents the largest group in terms of numbers of fish, but the fish are also very large in size, and hence fecundity, and can potentially contribute significant numbers of eggs to Smith Sound and adjacent areas. Smith Sound is considered the largest remaining spawning area for Northern Cod. Extensive eelgrass beds at the head of the Sound provide high quality nursery habitat. Much of the currently known spawning that occurs along the northeast coast appears to originate from migrating subgroups of cod which overwintered in Smith Sound (Templeman, 2007). Smith Sound cod aggregations may be critical to the recovery of the population (Templeman, 2007), although the potential role of bay stocks such as those in Smith Sound in rebuilding the offshore stocks is unknown (Rose, 2007). Given the importance of this population to one of the two major stocks within the LOMA, we have selected a score of 6. Atlantic cod are listed in the CP document as an ‘ecologically significant species’ (add one point). Score 7 3 Sensitivity: (3 + 3 + 7)/3 = 4.3 Risk of Harm: 0.36 x 4.3 = 1.5 Certainty Checklist Answer yes or no to all of the following questions. Record the number of NO’s to the 9 questions, and record certainty according to the scale provided below: 1 No’s = High certainty 2- 3 No’s = Medium certainty >4 No’s = Low certainty Y/N N Is the score supported by a large body of information? N Is the score supported by general expert agreement? N Is the interaction well understood, without major information gaps/sources of error? Y Is the current level of understanding based on empirical data rather than models, anecdotal information or probable scenarios? N Is the score supported by data which is specific to the region, (EBSA, LOMA, NW Atlantic? Y Is the score supported by recent data or research (the last 10 years or less)? N Is the score supported by long-term data sets (ten years or more) from multiple surveys (5 years or more)? Y Do you have a reasonable level of comfort in the scoring/conclusions? N Do you have a high level of confidence in the scoring/conclusions? Certainty Score: Low For interactions with Low certainty, underline the main factor(s) contributing to the uncertainty Lack of comprehensive data Lack of expert agreement Predictions based of future scenarios which are difficult to predict Other (provide explanation) Suggest possible research to address uncertainty: Improved enforcement and analysis of data in relation to reporting lost nets 4 Reference List 1. Halpern, B. S., Walbridge, S., Selkoe, K. A., Kappel, C. V., Micheli, F., D'Agrosa, C. et al. (2008). A Global Map of Human Impact on Marine Ecosystems. Science, 319, 948-952. 2. Lawson, G. L. & Rose, G. A. (2000). Seasonal distribution and movements of coastal cod (Gadus morhua L.) in Placentia Bay, Newfoundland. Fisheries Research, 49, 6175. 3. National Academy of Sciences (2008). Tackling Marine Debris in the 21st Century. 4. Rose, G. A. (2007). Cod: The Ecological History of the North Atlantic Fisheries. Breakwater Books. 5. Templeman, N. D. (2007). Placentia Bay-Grand Banks Large Ocean Management Area Ecologically and Biologically Significant Areas (Rep. No. 2007/052). Canadian Science Advisory Secretariat Research Document, Fisheries and Oceans Canada. 5 Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound Increased storm events Magnitude of Interaction Areal extent: Smith Sound is a small area which supports a very dense aggregation of cod. A deep (200m) trench provides over-wintering habitat for pre-spawning fish, and as deep waters cool in the spring, warming surface layers provide above zero waters if deep water should fall below optimal temperatures for spawning and survival of cod. Thus, during the spawning season, cod may be seen throughout Smith Sound. Figure 1. Cod distributions in Trinity Bay from acoustic surveys (O'Driscoll et al., 2000) Increased storm events are an escalating stressor related to climate change which is predicted to impact the LOMA. Score 10 Contact: Storm events affect the entire water column in shallow coastal areas, and therefore contact will be high for CPs associated with coastal areas (Fisheries and Ocean Canada, 2007) Score 10 Duration: The majority of cod return to Smith Sound during the winter (November-April), although some fish remain in the sound year-round (6 months). Juvenile fish remain in eelgrass beds at the head of the Sound, or in other suitable nursery habitat such as kelp beds throughout the year. Since this CP refers to the entire life cycle of cod in Smith Sound we have consider the CP to be present 12 months of the year. Super-cooling events resulting from storm mixing are most likely in the spring of the year when ice cover (which prevents wind related mixing) is gone, but surface waters are below 0oC (March-April)- but these events are not expected to occur annually. Chronic stressors which are unlikely to occur annually are scored in the low range. We have selected a score at the low end of the range to reflect the anticipated low frequency and duration of the stressor. Score 1 Intensity: Atlantic tropical cyclones are getting stronger on average, with a 30-year trend that has been related to an increase in ocean temperatures, and are predicted to impact the NW Atlantic at a high level of intensity relative to other areas of the globe (Elsner et al., 2008). The years 1995-2000 experienced the highest level of North Atlantic hurricane activity in the reliable record (Goldenberg et al., 2001). The largest increase in hurricanes reaching categories 4 and 5 occurred in the Pacific and Indian Oceans, but the highest increase in the number of cyclones and cyclone days occurred in the North Atlantic (Webster et al., 2005). The relationships between a warming environment and increasing storm events is complex, and research results and predictions are variable, and more research is clearly required (Emanuel, 2005; Emanuel, 2000; Goldenberg et al., 2001; Webster et al., 2005). Based on the available information we have selected a score at the low end of the high range. Score 7.5 Magnitude of Interaction: (10 x 10 x 1 x 7.5)/1000 = 0.75 Sensitivity Sensitivity of the CP to acute impacts: It is not clear exactly what factors contribute to making Smith Sound a unique spawning area for northern Atlantic cod, but the abundance of prey, particularly capelin, refuge from the intense fishing effort that led to the decline of offshore stocks, as well as the deep (200m) trench within a sheltered sound which offers over-wintering habitat for prespawning aggregations, are likely important factors. Spawning in Smith Sound begins in early April and continues into the summer, with spawning observed as late as July in some years (Rose, 2007). Some fish appear to remain in Smith Sound all year, but the majority migrate seasonally in and out of the bay. In a normal year, migrating cod return to Smith Sound in late fall or early winter when deep waters in the trench are warm (3-5oC). As spring approaches, deep waters cool, but temperatures are still above 0oC when cod begin to spawn in early April. By late May, temperatures in deep waters may dip below 0oC and the fish either move up into the warming surface waters or out into adjacent areas (Rose, 2007). An increase in storm surges can potentially led to super-cooling events during severe winter storms where the motion keeps seawater in a liquid state at temperatures well below -2oC and can lead to mass mortalities. In the spring of 2003, the normal cooling of the deep waters accelerated quickly in early April, trapping cod in sub-zero waters deep in the Sound, and about 5% (500,000 fish) froze to death in the super-cooled water (Rose, 2007). This type of event is rare, occurring when specific environmental conditions coincide, and may never occur again, but increased storm events may increase the risk of reoccurrence, although the additional risk is considered low (3). Score 3 Sensitivity of the CP to chronic impacts: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod which was assessed by COSEWIC in 2003 and designated endangered. The Status Report lists fishing (including legal, illegal and unreported catches) and fishing-induced changes to the ecosystem as key threats to cod recovery. Inshore components of the stock appear more productive than offshore components. Stewardship fishery catch rates in 2006-07 were slightly higher than in earlier fisheries between 1998 and 2002, and sentinel fisheries catch rates near Trinity Bay (southern 3K and northern 3L) have generally increased since 2002 and are currently above average for the time series. A pre-recruit index suggests that the strength of the 2003-2006 year-classes will be much lower than those that have supported recent fisheries (Fisheries and Oceans Canada, 2008). Mortality from the 2003 super-cooling event were significant (500,000 fish), but are sustainable (5% of biomass) provided other mortality sources are adjusted in consideration of the loss for the year in which the event occurred (score 2). Atlantic cod are listed in the CP document as a ‘depleted and rare species’, and will therefore rank higher on this scale than other CPs because they are already in need of recovery (add one point). Score 3 Sensitivity of ecosystem to harmful impacts to the CP: Smith Sound cod belong to the Newfoundland and Labrador population of Atlantic cod, one of two major cod stocks within the LOMA. Cod have historically had a huge influence on the ecosystem of the LOMA, mainly because of their large biomass and broad distribution compared to other species, and their significant role as both predator and prey at all trophic levels as they grow and move from one trophic level to another. Even though they are currently at less then one percent of their former biomass, they still represent a significant component of the total goundfish population. Since the sharp decline in cod biomass in the 1990s, stocks of invertebrates such as shrimp and crab have expanded to record highs in what has been termed a trophic cascade. These changes have been blamed on over-fishing resulting in perturbations to the predator-prey systems, and although environmental change may have had a contribution, it is clear that the role of Atlantic cod in the ecosystem is highly significant to its structure and function. Coastal bays provide significant spawning, nursery and over-wintering habitat for Atlantic cod within the LOMA. Since the collapse of the cod stocks in the early 1990s, much of the remaining biomass has been concentrated in coastal regions. Although cod were historically known to over-winter and spawn in these coastal areas, the recent concentration of cod in coastal bays, in contrast to the dearth of fish in adjacent shelf regions, may be without precedent (Lawson & Rose, 2000). Bay stocks are seen by many as a key component in the recovery of cod stocks within the LOMA as a whole. Smith Sound is an important overwintering area for the severely depleted population of Northern cod. The very dense aggregation of fish in the relatively small geographical area of Smith Sound during the winter not only represents the largest group in terms of numbers of fish, but the fish are also very large in size and hence fecundity, and can potentially contribute significant numbers of eggs to Smith Sound and adjacent areas. Smith Sound is considered the largest remaining spawning area for Northern Cod. Extensive eelgrass beds at the head of the Sound provide high quality nursery habitat. Much of the currently known spawning that occurs along the northeast coast appears to originate from migrating subgroups of cod which overwintered in Smith Sound (Templeman, 2007). Smith Sound cod aggregations may be critical to the recovery of the population (Templeman, 2007), although the potential role of bay stocks such as those in Smith Sound in rebuilding the offshore stocks is unknown (Rose, 2007). Given the importance of this population to one of the two major stocks within the LOMA, we have selected a score of 6. Atlantic cod are listed in the CP document as an ‘ecologically significant species’ (add one point). Score 7 Sensitivity: (3 + 3 + 7)/3 = 4.3 Risk of Harm: MoI x S = 0.75 x 4.3 = 3.2 Certainty Checklist Answer yes or no to all of the following questions. Record the number of NO’s to the 9 questions, and record certainty according to the scale provided below: 1 No’s = High certainty 2- 3 No’s = Medium certainty No’s = Low certainty >4 Y/N N Is the score supported by a large body of information? N Is the score supported by general expert agreement? N Is the interaction well understood, without major information gaps/sources of error? N Is the current level of understanding based on empirical data rather than models, anecdotal information or probable scenarios? N Is the score supported by data which is specific to the region, (EBSA, LOMA, NW Atlantic? N Is the score supported by recent data or research (the last 10 years or less)? N Is the score supported by long-term data sets (ten years or more) from multiple surveys (5 years or more)? Y Do you have a reasonable level of comfort in the scoring/conclusions? N Do you have a high level of confidence in the scoring/conclusions? Certainty Score: Low For interactions with Low certainty, underline the main factor(s) contributing to the uncertainty Lack of comprehensive data Lack of expert agreement Predictions based of future scenarios which are difficult to predict Other (provide explanation) Suggest possible research to address uncertainty: Improved regional monitoring Reference List 1. Elsner, J. B., Kossin, J. P., & Jagger, T. H. (2008). The increasing intensity of the strongest tropical cyclones. Nature, 455, 92-95. 2. Emanuel, K. (2005). Increasing Destructiveness of Tropical Cyclones over the past 30 Years. Nature, 436, 686-688. 3. Emanuel, K. A. (2000). A Statistical Analysis of Tropical Cyclone Intensity. Mon.Wea.Rev., 128, 1139-1152. 4. Fisheries and Ocean Canada (2007). Conservation Harvesting Plan (CHP), Atlanticwide for Mobile Gear Vessels 65-100', February 8, 2007 (unpublished) Fisheries and Oceans Canada, Newfoundland & Labrador Region. 5. Fisheries and Oceans Canada (2008). Stock Assessment of Northern (2J3KL) Cod in 2008 (Rep. No. 2008/034). Canadian Science Advisory Secretariat Science Advisory Report, Newfoundland and Labrador Region. 6. Goldenberg, S. B., Landsea, C. W., Mestas-Nunez, A. M., & Gray, W. M. (2001). The Recent Increase in Atlantic Hurricane Activity: Causes and Implications. Science, 293, 474-479. 7. Lawson, G. L. & Rose, G. A. (2000). Seasonal distribution and movements of coastal cod (Gadus morhua L.) in Placentia Bay, Newfoundland. Fisheries Research, 49, 6175. 8. O'Driscoll, R. L., Rose, G. A., Andersdon, J. T., & Mowbray, F. (2000). Spatial association between cod and capelin: a perspective on the inshore-offshore dichotomy (Rep. No. 2000/083). 9. Rose, G. A. (2007). Cod: The Ecological History of the North Atlantic Fisheries. Breakwater Books. 10. Templeman, N. D. (2007). Placentia Bay-Grand Banks Large Ocean Management Area Ecologically and Biologically Significant Areas (Rep. No. 2007/052). Canadian Science Advisory Secretariat Research Document, Fisheries and Oceans Canada. 11. Webster, P. J., Holland, G. J., Curry, J. A., & Chang, H. A. (2005). Changes in Tropical Cyclone Number, Duration, and Intensity in a Warming Environment. Science, 309, 1844-1846. Summary Table: Northern Atlantic cod spawning, nursing, migration, and refuge in Smith Sound. Certainty Key as cs es a c d i S MoI Risk Activity/Stressor (a x c x d x i) (as+cs+es) of 1000 3 Harm Gillnets 10 7.5 4.2 4 6.8 6 7 1.3 6.6 8.6 Med (groundfish) Recreational 10 7.5 1 4 7.5 8.5 7 0.3 7.7 2.3 Med cod fishery Ghost nets 1.5 4 10 6 3 3 7 0.36 4.3 1.5 Low Increased 10 10 1 7.5 0.75 3 3 7 4.3 3.2 Low storm events Cumulative CP Score 15.6