Toxic dinoflagellates: introduction of potentially harmful dinoflagellates due to ballast water in Eastern Canada

Similar documents
REVIEW OF ALTERNATE BALLAST WATER EXCHANGE ZONES FOR VESSEL TRAFFIC TO NEWFOUNDLAND AND LABRADOR AND THE CANADIAN ARCTIC

Arctic stowaways: the potential for species introduction to occur in Svalbard associated with shipping Progress report January 2012

Testing for Grazer Adaptation to Toxic Algae

Ireland: Current Conditions

Harmful Algal Blooms (HABs) 5 Applications

Future climate impacts on Puget Sound oceanography: the North Pacific and hydrological context

Greenhouse Effect & Global Warming

Phytoplankton. Zooplankton. Nutrients

Ireland: Current Conditions

Ireland: Current Conditions

4.3 Climate (6.3.3) Explore this Phenomena. The same sun shines on the entire Earth. Explain why these two areas have such different climates.

CHAPTER IV THE RELATIONSHIP BETWEEN OCEANOGRAPHY AND METEOROLOGY

Management of recreational waters in relationship with harmful microalgae blooms (HAB) in the Mediterranean Sea

KCC White Paper: The 100 Year Hurricane. Could it happen this year? Are insurers prepared? KAREN CLARK & COMPANY. June 2014

1990 Intergovernmental Panel on Climate Change Impacts Assessment

A Planned Course Statement for. Oceanography. Course # 410 Grade(s) 9, 10, 11, 12. Length of Period (mins.) 40 Total Clock Hours: 60

Recent Harmful Algal blooms (HABs) Events in Indonesia

Coastal Impacts of Climate Change in the Northwest: A Summary of the Findings of the upcoming National Climate Assessment

Figure 14 p.385 5/11/2016. Plankton Production and Food Webs. Plankton Production and Food Webs

How long can zebra mussels survive out of water? A math model!

West Coast HABs affect:

Ireland: Current Conditions

Ocean Zones How are the intertidal, neritic, and oceanic zones different?

Marine Primary Producers. Primary production

CBA Practice Exam - Ecology

A Synthesis of Results from the Norwegian ESSAS (N-ESSAS) Project

Observed changes in climate and their effects

Ireland: Current Conditions

53 contributors for 35 individual reports in 2009 show 5% of figures today

Chapter 8. Biogeographic Processes. Upon completion of this chapter the student will be able to:

Mid-season Storm Surge Update: December, 2013

4. In areas where tectonic plates collide, the seafloor has deep. 5. In areas where tectonic plates separate, the seafloor has mid- ocean

ATOC OUR CHANGING ENVIRONMENT

Ocean facts continued

THE CANADIAN CENTRE FOR CLIMATE MODELLING AND ANALYSIS

3.1 Distribution of Organisms in the Biosphere Date:

Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity?

Climate change projections for Ontario: an updated synthesis for policymakers and planners

1. Oceans. Example 2. oxygen.

FINAL EXAM PRACTICE #3: Meteorology, Climate, and Ecology

Ireland: Current Conditions

Climate change in the U.S. Northeast

Marine Ecology Pacing Guide

The Impact of Climate Change on the Intensity and Frequency of Windstorms in Canada

OCEANOGRAPHY. 13. Biological Productivity and Energy Transfer. Alessandro Grippo, Ph.D. part 2: Photosynthetic Marine Organisms

Biodiversity Classwork Classwork #1

David W. Seaborn 1, A. Michelle Seaborn 2, William M. Dunstan 2, and Harold G. Marshall 1

HAB Forecaster. For info on HABs in the Pacific Northwest see:

FLOW: Amigos de Bolsa Chica Citizen Science Program. Plankton Collection and Identification Report

Ireland: Predictions. NMP Current closures ASP AZP DSP PSP

December 23 rd, 2018 Sample Current Affairs

Arctic climate change and effects on the ecosystems

Primary Productivity (Phytoplankton) Lab

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans?

Weather and Climate Summary and Forecast January 2018 Report

INTERNATIONAL CONVENTION FOR THE CONTROL AND MANAGEMENT OF SHIPS' BALLAST WATER AND SEDIMENTS, 2004

Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.

6. What has been the most effective erosive agent in the climate system? a. Water b. Ice c. Wind

Ellen L. Mecray NOAA Regional Climate Services Director, Eastern Region Taunton, MA

Module 11: Meteorology Topic 6 Content: Severe Weather Notes

Diarrhetic shellfish poisoning in socio-economic perspective in Prymorsky region, Russia

Winter. Here s what a weak La Nina usually brings to the nation with tempseraures:

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are

CLIMATE READY BOSTON. Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016

Weather and Climate Summary and Forecast November 2017 Report

4th Grade Social Studies First Nine Weeks

EDUCATION PROGRAMS GUIDE

Oceans. Sea Surface Temperature. Sea Level. Ocean Heat INDICATORS IN THIS CHAPTER

DSP: This is currently a low risk period for early DSP events. All sites are currently below regulatory limits.

Distribution of Dinoflagellate Cysts in the Surface Sediment of the South China Sea, Area I: Gulf of Thailand and East Coast of Peninsular Malaysia

Chapter 14: Primary Producers

Shellfish biotoxin report (last week)

American Harris mud crab Rhithropanopeus harrisii

Contents. Preface. IC. Introductory Chapter. 1. The Ocean in the Earth System. Ocean Studies and Pedagogy Acknowledgments

Lesson th Grade * Teacher Prep. Photocopy New Assignment Log Portfolio 9

Ballast sediment-mediated transport of non-indigenous species of dinoflagellates on the East Coast of Canada

Unit 8 Test Review -- Oceanography

Microplastics in the marine environment of coastal British Columbia

FLOW: Amigos de Bolsa Chica Citizen Science Program. Plankton Collection and Identification Report

PRINCIPLE OF OCEANOGRAPHY PBBT101 UNIT-1 INTRODUCTION OF OCEANIC ENVIRONMENT. PART-A (2 Marks)

Atlantic Region s Changing Climate. Dr. Adam Fenech, University of Prince Edward Island Climate Change and Aquaculture Symposium 11 March 2014

DSP: This is currently a low risk period for early DSP events. All sites are currently below regulatory limits.

Coastal issues: Beaches and Estuaries

Here s what a weak El Nino usually brings to the nation with temperatures:

Ireland: Predictions. NMP Current closures ASP AZP DSP PSP

EQ: Discuss main geographic landforms of the U.S. & Canada and examine varied landforms in relation to their lifestyles.

Weather and Climate Summary and Forecast October 2017 Report

It s true, these activities are all facets of marine science. But they represent a pretty small part of the picture.

Winter Introduction to THE OCEANS

SEMESTER AT SEA COURSE SYLLABUS. Introduction to Oceanography

Landforms. Lesson 1: Physical Geography of Canada Mexico. Canada s mountainous eastern and western edges create a central region of fertile plains.

Adaptive Radiation (Lexile 990L)

Warm Up Vocabulary Check

Unit 1: Geography. For additional information, refer to this website: 1 G e o g r a p h y

Where is all the water?

3) What is the difference between latitude and longitude and what is their affect on local and world weather and climate?

Storms. 3. Storm types 4. Coastal Sectors 5. Sorm Location and Seasonality 6. Storm Severity 7. Storm Frequency and grouping 8. The design storm event

Climate Change and Arctic Ecosystems

Marine Primary Producers

PROF. DR HAB. PIOTR TRYJANOWSKI

Transcription:

Toxic dinoflagellates: introduction of potentially harmful dinoflagellates due to ballast water in Eastern Canada Jacqueline Modler, Undergraduate Student, Dalhousie University Abstract Ballast water frequently introduces potentially harmful, non-indigenous dinoflagellates into marine ecosystems, either through water or within ballast sediments. Foreign dinoflagellates contribute to the development of harmful algal blooms, and affect aquaculture and human health due to paralytic shellfish poison (PSP). Eastern Canadian marine ecosystems are becoming increasingly vulnerable due to rising water temperatures, enabling tropical dinoflagellates to survive in an environment that was previously too cold. Ships participating in a coastal ballast exchange have the highest probability of transporting harmful, non-indigenous dinoflagellates. This paper aims to prove that additional methods of control are needed to limit the number of harmful dinoflagellates transported by ballast water. Ballast water exchange, made law in 2006, is an insufficient method to control the introduction of foreign taxa, and when done in coastal waters, could instead increase the number of toxic dinoflagellates brought into marine ecosystems. The implementation of an external Canadian management body is proposed to regulate ballast water exchange and tighten ballast water requirements. Studies in Eastern Canada will be used to examine the magnitude of harmful, nonindigenous dinoflagellates introduced in Eastern Canada. As well, national and international studies will be brought together to examine potential effect of nonindigenous dinoflagellates. 1. Introduction Ballast water is responsible for the transportation of non-indigenous species (NIS) and potentially harmful dinoflagellates into marine ecosystems. In Eastern Canada, ballast water is particularly problematic due to a continual increase in both size and distribution of ship traffic (Roy et al. 2012). Bulk carriers dominate ship traffic along the eastern coast in Canada, with ships being divided among those that do and do not engage in ballast water exchange (BWE). Transoceanic ships, coastal ships with BWE, and coastal ships without ballast water exchange are the main categories of ships that visit Canada s eastern coast (Roy et al, 2012). Transoceanic ships (TOE) undertake ballast water exchange and voyage across continents. Coastal ships are those typically from the United States of America and they are further divided between those that do undergo a ballast water exchange (CE) and those that do not engage in a ballast water exchange (CNE). The importation of dinoflagellates via ballast water can be potentially harmful to marine ecosystems, having disastrous effects on fish communities, aquaculture and eventually, human health. Harmful dinoflagellate species are transferred through the ballast water, and increase frequency and severity of toxic poisoning towards humans, such as paralytic shellfish poisoning (PCP) (Casas-Monroy et al.,2011). By allowing harmful dinoflagellates to continue to increase in concentration, they can produce dangerous harmful algal blooms (HAB), producing toxins and causing mechanical damage to other organisms (Mudie et al.,2001). 28

Research today on the introduction of harmful dinoflagellates due to ballast water is lacking in longevity. Harmful dinoflagellate concentrations have only been studied for a few decades and long term effects are relatively unknown. Previous studies, such as Mudie et al (2001) utilized the Holocene history of dinoflagellate cysts as a proxy for production of harmful algal blooms. Some dinoflagellates are able to form cysts at various life stages which can be dormant or serve as seeds. Dormant cysts are better able to withstand adverse conditions and can help dinoflagellates to survive whereas, cysts that act as seeds will often initiate harmful algal blooms (Lacasse et al., 2012). Not all dinoflagellates produce seeds, which result in large margins of error in Mudie and al. study (2001). This paper illustrates the need for additional limitations for BWE ships. Ships with no BWE can account for over half of the foreign water discharged, and are primarily from regions where dinoflagellates have higher chances of survival, such as northeast USA (Lacasse et al., 2012). The purpose of this paper is to prove that stricter enforcement of BWE is needed. Studies from Eastern Canada will be brought together to examine the presence of NIS and harmful dinoflagellates brought into East Coast waters by ballast water. International studies will be used to outline potential effects of high concentrations of harmful dinoflagellates on the ecosystem and aquaculture. If achieved, limiting the amount of future harmful dinoflagellates will reduce the frequency and severity of harmful algae blooms allowing for a healthier marine ecosystem. Additionally, this paper strives to suggest the need for an external Canadian management body to control and improve upon current BWE practices. This management body would work to ensure that BWE is being done a proper distance away from the coast, and ensuring that it is done by all ships of proper size. It would also work to tighten the requirements for ships who do not need undergo a BWE. Currently there are international governing bodies and national rules but no active managing body for Canada. However, this management body would be limited in their ability by financial restrictions as well as the difficulty in tracking all ships entering and leaving all Canadian coasts. 2. Background Ballast water is seawater carried in ballast tanks of large ships for the purpose of increasing stability of a ship once cargo has been released or before it is loaded (Casas-Monroy et al., 2011). Ships take up water at or near port of departure and later discharge once near destination, in the process transporting many marine organisms. Some of the organisms introduced are potentially dangerous dinoflagellates, most commonly a form of marine plankton (Casas-Monroy et al., 2011). Dinoflagellates can cause harmful algal blooms, known as red tides, and when NIS arrive to the area they can invade existing ecosystems (Mudie et al., 2002). A large amount of ships containing ballast water undergo a ballast water exchange. A BWE occurs to replace the coastal ballast water with mid-ocean surface seawater, thus also exchanging organisms with in the water (Ruiz and Reid, 2007). Canada introduced BWE in the early 1990 s and by 2006 it was introduced as law (Roy et al., 2012). The law required all ships leaving Canada s coastal waters to undergo a full flush of their ballast water in the open ocean, away from coastal waters, before emptying ballast water in Canadian waters. Toxic dinoflagellates only distribute and have the potential to invade in coastal waters, 29

defending the idea that flushing ballast tanks would decrease the potential risks involving toxic dinoflagellates (Roy et al., 2012). Dinoflagellates have posed an expedited risk to aquaculture over the past 5-6 decades due to global changes. Canada has experienced an increase in ship traffic, driving an increase in harmful algal blooms (Mudie et al., 2001). Additionally, climate change is causing an increase in ocean temperatures, allowing the toxic, invasive dinoflagellates an advantage in the changing environment. Previously, cold water temperature reduced the chances of survival for dinoflagellates that originated from warmer waters. Warmer water along the Atlantic coast gives dinoflagellates improved chances of survival. Many invasive plants share traits that increase their ability to adapt to a transitioning environment (Dukes and Mooney, 1999). These traits will favor the invasive species over the non-invasive, increasing the potential for damage to the surrounding ecosystem. As ocean temperatures continue to increase, so does the vulnerability of Canada s eastern coast. 3. Ballast water exchange The introduction of NIS dinoflagellates relies on the dinoflagellate s ability to survive considerable time without light (Figure 1. Summarizes all necessary steps for successful dinoflagellate survival). Many dinoflagellate taxa are mixotrophic, meaning they can use a variety of sources for energy. This enables theme to feed on organic material found in ballast tanks when light is unavailable (Roy et al., 2012). Additionally, dinoflagellates can form temporary dormant cysts to endure a long travel, and later germinate in ballast tank or once introduced into ocean water. A study on the introduction of harmful dinoflagellates in Eastern Canada conducted by Roy et al. (2012) found that 56% of ships studied visiting the St Lawrence, Halifax, and St John ports contained NIS dinoflagellates, and most were found in ships that underwent BWE. Using 5L Nalgene bottles, samples were taken of ballast water though manholes of Transoceanic (TOE), coastal ships Figure 1. Flow chart of steps necessary for ballast water introduction (Hallegraeff, 1998). 30

with ballast water exchange (CE) and coastal ships without ballast water exchange (CNE). Some ships carry a small enough amount of water to not need to undergo a ballast water exchange, but still pose some risk to the environment (Ruiz and Reid, 2007). In these cases, the residual coastal water is released at the port and introduced directly into the destination s coastal water (Ruiz and Reid, 2007). Coastal ships that did not engage in a ballast water exchange contained smaller concentrations, and a lower number of NIS taxa than ships who underwent a ballast water exchange (TOE and CE) (Roy et al., 2012). The introduction of an external management body could ensure that ships who undergo BWE do so at a sufficient distance away from the coast in order to properly flush out the tank with surface water. Doing so would ideally reduce the amount of NIS dinoflagellates that enter Eastern Canada through ballast water exchanging ships. Another study conducted by Casas-Monroy et al. (2011) examined the ballast water sediments of cargo ships visiting the east coast of Canada. This was the first study in the area to examine phytoplankton in ballast sediments. The study dealt with dinoflagellate cysts, both live and empty, as empty cysts may represent germination that occurred on board. Cyst samples were taken from ballast water tanks when empty, and cysts were divided into categories of viable cysts, empty cysts, total cysts, total NIS cysts, empty NIS cysts and viable NIS cysts. Of all taxa examined, 7 were potentially harmful or toxic and 14 were non-indigenous to the area (pictured below in Figure 2). Living and potentially viable cysts of NIS were present in 30% of ships studied, found in higher Figure 2. Non-indigenous species found in ballast sediments on the east coast of Canada (Casas-Monroy, 2011). concentrations in ships without ballast water exchange (Casas-Monroy et al., 2011). The studies of Roy et al. (2012) and Casas-Monroy et al. (2011), come to inconclusive results on the efficiency of BWE. Roy et al. (2012), concludes that ballast water exchanging ships have increased concentrations of NIS dinoflagellates. In contrast, Casas-Monroy et al. (2011) had higher concentrations of all dinoflagellate cysts in ships that did not engage in BWE. However, it did acknowledge that ballast sediments do introduce NIS, and the location of BWE is important. Ballast exchange occurring away from the coast reduces the amount of sediment and relating organisms in comparison to ballast exchange in coastal waters. By flushing the ballast tank with mid-ocean 31

water, most of the coastal water and sediments are removed. And because the mid-ocean water is closer to the surface than the original coastal water, less sediments remain in the ballast tank once the ship ahs arrived at the destination (Ruiz and Reid, 2007). Both studies arrive at a mutual conclusion that coastal ships exchanging ballast water have the highest chance of introducing harmful, NIS into Eastern Canadian waters. Distance of travel is another factor contributing to the increase of NIS dinoflagellates in coastal ships. Although Roy et al. (2012) found no clear relation between shorter transit times and lower cell concentrations, it likely contributed to species survival. Shorter trips favour the survival of dinoflagellate cysts, and result in higher concentration of potentially viable cysts found in continental ships (Casas-Monroy et al., 2011). This is true for any tank species, as the age of ballast water increases, the survival rate of species decreases. In a study conducted by Bunkholder et al. (2007), after 33 days no culturable phytoplankton were found. As size and speed of ships continues to increase, along with it the potential for NIS to remain viable once in Eastern Canada. An external ballast water management body would be able to control dinoflagellate introduction due to ballast water. Management would be able to track and ensure that all BWE is being done away from the coast using mid-ocean surface waters. This could greatly decrease dinoflagellate introduction from coastal ballast water exchanging ships. Additionally, a management body has the ability to track the duration of the trip and control if the probability of introducing live dinoflagellates is too high. 4. Temperature on viability The cold water in Eastern Canadian waters are beneficial for limiting the survival of some nonindigenous dinoflagellates. Transoceanic ships from tropical waters transport dinoflagellates unable to endure cold waters. The greatest threat of NIS dinoflagellates to Eastern Canadian waters are those also from cold water such as from the North American Atlantic coast (Claudi and Ravishanker, 2006). These taxa are most commonly within a transportation distance that does not require BWE, which increases their chance of remaining viable. Unfortunately, due to global warming and climate change, ocean temperatures are rising and oceans are becoming more susceptible to invasions of NIS. The study by Roy et al. (2012) found not previously reported, harmful dinoflagellates that originate from tropical waters, confirming that increasing water temperatures are increasing the potential for tropical species to invade. As water temperatures increase, the need for an external ballast water management body becomes more important, because the potential for dinoflagellate invasions increases (Roy et al., 2012). 5. Effects of toxic non-indigenous species on aquaculture and ecosystems Harmful algal blooms (HAB), commonly referred to as red tides occur when a single phytoplankton species rapidly accumulates and negatively impact the environment. Toxic dinoflagellates harm zooplankton and their predators, and if plankton species are not able to avoid the toxin they are susceptible to starvation and the loss of oxygen. The most harmful and widespread red tides caused by toxic dinoflagellates can result in human illness (Mudie et al., 2002). Paralytic shellfish poisoning (PSP) results from shellfish products contaminated with toxins 32

from 11 different species of dinoflagellates, and has been observed in alarming increasing frequency (Hallegraeff, 1998). Concentrations of diarrheic shellfish poison (DSP) toxic producing algae reached hundreds to thousands in 60% of potentially harmful species (Roy et al., 2012). The aquaculture industry faces enormous losses from toxic dinoflagellate caused illnesses. PSP alone resulted in over $4 million of losses per outbreak in the 1970 s-1990 s and has likely risen to this date (Taylor, 1993). Coastal shipping contributes to secondary coastal spreading of NIS organisms (Cordell et al., 2009). Once a single tropical dinoflagellate taxon has managed to survive in a colder, temperate ecosystem it enables the continuation of invasion. In the Halifax port, Neocratium furca and Gonyaulax scrippase showed high levels of abundance and occurrence (Roy et al., 2012) both species being largely harmful during the development of red tides. 6. Conclusion Harmful dinoflagellate species are being introduced into Eastern Canadian waters largely through the use of ballast water. Though ballast water exchange (BWE) was introduced as law in 2006 to force transoceanic and some coastal ships to undergo a BWE away from coastal waters, its efficiency has been largely disputed (Roy et al., 2012). Coastal ships have the highest potential for transporting harmful, NIS due to both less time travelled in the ballast tank, and originating in an ecosystem more similar to that of Eastern Canada. BWE performed in open ocean decreases ballast sediment and potentially viable dinoflagellate cysts (Casas-Monroy et al., 2011). Previous studies were done to quantify the number of toxic dinoflagellates introduced into Eastern Canada by different types of ballast water exchanging ships. Eastern Canadian waters are becoming more favorable to the invasion of harmful, NIS dinoflagellates due to an increase in the shipping industry and an increase in water temperature. As shipping increases and ships becomes faster, more opportunities are presented for NIS to withstand the length of travel and remain viable until destination. Future studies should explore how specific indigenous species react to the introduction of both harmful and non-harmful, NIS dinoflagellates, and if they are affected by ocean acidification. Increasing ocean temperatures in Eastern Canada due to global warming will enable the survival of new non-indigenous dinoflagellate taxa from more tropical environments. It is important to determine how existing species will react to the introduction of these new species. Harmful, NIS dinoflagellates pose a threat to Eastern Canadian ecosystems as well as human health that is only expected to increase. It would be beneficial to investigate new methods to limit BWE, such as only exchanging mid-ocean, and perhaps not having coastal ships engage in ballast water exchange. These methods could eliminate many possibilities for the transfer of NIS and reduce related harmful algal blooms and illnesses. This paper aims to suggest that the implementation of an external Canadian management body to control and improve upon current BWE practices would better the current situation. This management body could help to limit coastal BWE and ensure that ballast water tanks are being flushed with mid-ocean surface water. By implementing a management body the amount of harmful NIS dinoflagellates brought by coastal ballast water exchange could be greatly reduced. 33

References Burkholder JM, Hallegraedd GM, Melia G, Cohen A, Bowers HA, Oldach DW, Parrow MW, Sullivan MJ, Zimba PV, Allen EH, Kinder CA, Mallin MA. 2007. Phytoplankton and bacterial assemblages in ballast water of U.S. military ships as a function of port of origin, voyage time and ocean exchange practices. Harmful Algae. 6(4): 486-518. Casas-Monroy O, Roy S, Rochon A. 2011. Ballast sediment-mediated transport of non-indigenous species of dinoflagellates on the East Coast of Canada. Aquatic Invasions. 6(3): 231-248. Claudi R, Ravishankar TJ. 2006. Quantification of risk of alien species introductions associated with ballast water discharge in the Gulf of St Lawrence. Biol Invasions. 8(1): 25-44. Cordell JR, Lawrence DJ, Ferm NC, Tear LM, Smith SS, Herwig RP. 2009. Factors influencing densities of non-indigenous species in the ballast water of ships arriving at ports in Pugent Sound, Washington, United States. Aquatic Conserv Mar Freshw Ecosyst. 19(3): 322-343. Dukes JS, Mooney H. 1999. Does global change increase the success of biological invaders?. Trends Ecol Evol. 14: 135-139. Hallengraeff GM. 1998. Transport of toxic dinoflagellates via ships ballast water: bioeconomic risk assessment and efficacy of possible ballast water management strategies. Mar Ecol Prog Ser. 168: 297-309. Lacasse O, Rochon A, Roy S. 2012. High cyst concentrations of the potentially toxic dinoflagellate Alexandrium tamarense species complex in Bedford Basin, Halifax, Nova Scotia, Canada. Mar Pollut Bull. 66: 230-233. Mudie PJ, Rochon A, Levac E. 2002. Palynological records of red tide-producing species in Canada: past trends and implications for the future. Palaeogeogr Palaeocl. 180:159-186. Roy S, Parenteau M, Casas-Monroy O, Rochon A. 2012. Coastal ship traffic: a significant introduction vector for potentially harmful dinoflagellates in eastern Canada. Can J Fish Aquat Sci. 69: 627-644. Ruiz, G.M. and Reid, D.F. eds., 2007. Current state of understanding about the effectiveness of ballast water exchange (BWE) in reducing aquatic nonindigenous species (ANS) introductions to the Great Lakes Basin and Chesapeake Bay, USA: synthesis and analysis of existing information. US Department of Commerce, National Oceanic and Atmospheric Administration. Taylor FJR. 1993. Current problems with harmful phytoplankton blooms in British Columbia waters. In: Smayda TJ, Shimizu Y. (Eds.), Toxic Phytoplankton Blooms in the Sea. Elsevier Scientific Publications, Amsterdam, pp. 699-703. 34