Category Archives: Lakes

Night Paddling Ireland’s Rare Saltwater Lake, Lough Hyne, June 2019

June 21st, the summer solstice. Ten thirty. Night descended like an elaborate dimmer on an antique lamp. Dark, looming ledges leaned over the rare, saltwater lake. My eyes adjusted to barely imperceptible shifts of light as I paddled a two-man kayak through ever-darkening water. Warm, syrupy salted air filled my lungs and swirled around the elderberry cough drop I sucked to keep from coughing. Pneumonia gripped my back and I sat erect, strapped and locked into the skirt of my waterproof waders. Still, water drizzled down my back and I tried to ignore it. I wished more than anything I wore my swimsuit, instead of this neoprene—and that I was swimming. But then I whispered to the lake—I am grateful. This is beautiful. I’m alive. I am so lucky.

Bats swooped. Grey herons shrieked and cackled. Their loud, ear-piercing night calls made my paddling partner, an accountant from Chicago, ask nervous questions from the stern of our kayak. She worried. “Will we get pulled out to sea?” I assured her, “the passageway is way over there. We’re not going anywhere near it, and besides, it’s so narrow, it’s only big enough for a seal to swim through.” “Or a kayak,” she quipped. “Don’t worry,” I said, a bit disappointedly, “we’re not going out to sea.” And we weren’t going out to sea. We paddled away from the direction of the Rapids, a narrow opening in the lake that bordered Barloge Creek, which then broadened into a harbor out onto the Wild Atlantic.

Lough Hyne, Co. Cork, Ireland. Stetson photo

Several months in advance, I’d planned my trip to Ireland with the intention of paddling Lough Hyne, located almost five kilometers from Skibbereen on the southwest coast of Ireland. I’d arrived by electric car, having driven from the small village of Durrus, which should have been a 45-minute drive–according to Google maps, GPS and my guidebooks of the Wild Atlantic Way. By that night, I’d already been driving in southwest Ireland for five days, and had gained the confidence to pass a tractor, drive 80 kilometers per hour (barely 50mph) on curvy back roads between Durrus and Skibbereen—where gut instinct battled confusing GPS commands, and swear in Irish. I’d converted.

When I first arrived at the lake’s launch and parking area, my jaw dropped. A deep azure uninterruptible sky splashed like a reflection over the pretty blue lake. It’s roughly sixty hectares in area, or 150 acres, but splendidly rich in surprises, hidden coves and rock caves, strange myths and an island of castle ruins, an ancient home to a shameful king, an Irish version of the Emperor’s New Clothes. A group assembled beside the launch, practiced paddling in the air, introducing ourselves. One woman and her granddaughter traveled from Perle, Australia to experience night-time paddling on Lough Hyne, an item on her “bucket list,” she told me. As we struggled to climb into waterproof gear—several layers of thick neoprene overalls and hip-waders—that doubled as a skirt attached to the kayak—and strapped life vests over large busts—the four of us women lamented how unnecessary all of this waterproof gear felt.  Just minutes before we selected our boats, two local swimming clubs waded into the lake. The Lough Hyne Lappers wore wetsuits. The other group—the one I wanted to join—wore togs, what Americans call swimsuits. These women called themselves the Dippers, an inside joke. They swam in their togs for a good while—long enough for our kayaking guides to run through the safety protocols, and to assist paddlers with their gear. We resembled trainees in Willie the Whale costumes at an amusement park. I’m glad that no one was allowed to take pictures—we were all required to hand over cameras, cell phones, car keys and watches to put in a safety box until after we returned from paddling. We launched the kayaks around ten o’clock at night and returned well after midnight. (We were not allowed to take our cameras or phones while kayaking.)

Swimmers and paddlers at Lough Hyne, Co. Cork, Ireland in June 2019. Stetson photo

As we paddled away from the launch in the remaining daylight, I noticed a dreamy rose-colored house that sat nestled in the trees along the shore. Once home to a lord, the 1830 Regency-style Lough Ine House rents for €500 a night in June, complete with a private beach and a small cottage on a 15-acre estate. I spotted an overturned canoe resting beside a little dock but I didn’t see anyone. Immediately, I imagined characters from Daphne du Maurier’s Rebecca: a shy heroine bending to cut roses in the patio garden for a vase in the library; a brooding anti-hero sulking irresistibly in one of the upstairs windows overlooking the lake and the sea beyond. This was one of the many moments I told myself, “One day, I shall live here, and write a book.” (Or, write something, I thought!)

Stetson photo

In pitch black darkness, we could only see the red glowing flashing light on the back of the guides’ headlamps, and the fireworks of bioluminescence streamed like comets from a dozen boats. Like silent firecrackers exploding underwater, microscopic organisms called dinoflagellates, a group of microalgae that act like animals, swim vertically in the water column to feed. Dinoflagellates feed at night. Pulling my paddle through invisible water, I excited these strange little plant creatures. Minature Swampthings. I remembered collecting some of the same dinoflagellates at Kettle Cove State Park in southern Maine. After collecting specimens in a “plankton tow” with a marine net, I inspected a few of the same species abundant in Casco Bay, Maine that marine scientists study in Lough Hyne. Ceratium furca and Ceratium fusus were two such armored species, both characterized by long horn-like bodies—which fascinated my classmates under a microscope—but truly awed and inspired everyone paddling in Lough Hyne with red and blue flashes of bioluminescence. If you’d like to know more about microalgae, see my previous post.

Lough Hyne, in the early evening before dark. Stetson photo

Since the lake is tidally-fed, the Lough is entirely populated by marine species. It was Europe’s first marine reserve. Now it’s a destination for night-time kayakers, marine biologists who study abundant communities of microalgae, the fabled (and very real) five-foot-long lobsters and giant sea stars, and the blue carbon potential of an eelgrass bed in the creek. One of the kayaking guides, Ryan, told me about his master’s degree project on the local eelgrass, and we chatted about the latest carbon sequestration science on salt marshes and eelgrass—called “blue carbon.” Eelgrass is a submerged aquatic flowering plant, a true sea grass with inconspicuous flowers. It spends most of its life submerged, swaying in the ebb and flow of tidal inlets and estuaries in the intertidal zone; its meadows, or beds, capture carbon, and hold onto it, just as salt marshes do. They are quiet climate avengers, in a way.

As we paddled around the perimeter of the lake, circumnavigating the island of castle ruins, we explored rock caves and listened to one of the guides, a graduate student at UCC, tell us about the holy well, Tobarín Súl, situated just beyond our reach. The Lough Hyne holy well draws believers who leave behind their white canes and old glasses—since they’d no longer need them after “doing the rounds,” walking twelve times clockwise around the holy well. Each of the holy wells in Ireland is known for curing (or causing) health issues related to a specific body part. If a believer wanted to curse another person, she or he need only to “do the rounds” counter-clockwise twelve times to cause the ailment, and in the case of the Lough Hyne holy well, might inflict conjunctivitis or blindness, or stink eye.

Once back at the launch, our paddling party stripped out of the neoprene gear as a bearded man announced, “It’s officially my birthday. I’m seventy! Which of you ladies wants to go skinny dipping?” A few laughed. I got scientific. “That would be quite psychedelic! Our bodies would sparkle and glow with the bioluminescence of dinoflagellates! You know—“ No one was interested in the science. Someone liked the idea of glowing bodies and “seeing sparks” but I bantered on, a little ditzy from cold and flu medicine, and antibiotics: “Well, they do reproduce sexually in adverse conditions—that’s why they’re shooting off the light. We interrupted. They were feeding—and…” Only the accountant from Chicago remarked, “Wow, you’re so passionate about this nature-y stuff.” We helped each other out of the gear while the bearded birthday man watched, a little more than disappointed no one was going to go skinny-dipping. I said, “This explains a lot…” and he said, “The Irish invented voyeurism!”

The cool, dark drive back to Durrus on curvy back roads both exhilarated my nerves and tested my courage. No street lights aided; only my headlights and the GPS—and my inner compass guided my way. I had to turn around twice—once when I came to a four-way intersection with no visible signage, and a second time as I pulled erroneously into the driveway for the Maulinward Burial Ground. I second-guessed myself there—and thought, “Is this a sign—a spiritual sign? Like a dark night of the soul sign?” I turned around, and eventually crept silently in my electric rental car down a dirt road.

Durrus, Co. Cork. Stetson photo

The moment I smelled horses—that wholesome meadow-sweet animal scent, I knew I’d come home. On my first night, I’d walked down that dirt road and came nose-to-nose with a mare on the other side of a fence lined with hot pink foxglove. She had a foal just old enough to walk but young enough that it hid behind its mother’s hind legs, staring at me. I talked to the mare in clicks and cries of joy, and sighs—like we were old friends, exchanging gossip from the field. On my last night in Durrus, there was a storm—a wild, windy torrential rain. Tree branches, leaves and flower blossoms danced chaotically through the garden like creatures out of Oz, or fairy land. I spent that last Sunday inside, watching the storm, sipping lemon tea and listening to the sounds of the Four Mile Water falls rushing over the road.

Four Mile Waters in Durrus, Co. Cork, Ireland. Stetson photo

If you’re interested in sea kayaking in this part of Co. Cork, Ireland, and want to paddle at night on Lough Hyne like I did, you can find out how to do this with Atlantic Sea Kayaking.

Healthy Waters Coalition – What’s on Our Minds, In Our Hearts

At my Healthy Waters Coalition meeting tonight, where we discussed the value of accurate, balanced information about oil spill prevention, I accidentally spilled pink lemonade across the agenda.  (From now on, the incident will be remembered as the “pink spill,” and it can be added to a long list of funny things I have done while leading coalition meetings.) I began to think about what’s really motivating our efforts to inform and educate Sebago Lakes Region citizens and local businesses about watershed issues.

We are a water-based economy here in this part of southern Maine. Boat rentals and recreation-based businesses, real estate and restaurants, florists and landscaping contractors, summer camps for children and accommodations (think: Inn by the Pond), not to mention waterfront property in towns–and property taxes paid to Towns–all bring in millions of dollars in annual revenue for the Sebago Lakes Region. The State of Maine tracks the annual revenue for freshwater fishing and accommodations for several Lakes Region towns. Wetlands are valued for their ecological services, too, and that translates to dollars. Real dollars. Wetlands attenuate flooding and aid in filtering waters to provide good water quality in our groundwater, which produces the drinking water for those who have private wells.  All of the headwater streams (94-100% of streams) in the region are located in Source Water Protection Areas (SPAs), meaning that they directly feed into a public drinking water system. In our region, that system is Sebago Lake, which is so clean, it’s exempt from the federal filtration requirement, an expensive option if ever it were to become necessary for the Portland Water District to put in place.

I want to reach out to other groups engaged in an open dialogue about the possible transportation of oil sands through New England and the importance of protecting our local watersheds, local economy–as the two are interconnected.  While the HWC already has members in 8 Lakes Region towns, representatives from local government boards and committees, watershed organizations, local businesses and other interests, such as Saint Joseph’s College, and we have partnered with some fantastic environmental and conservation-oriented nonprofit organizations already, I’d like to connect the Healthy Waters Coalition with a broader network.  I’m interested in connecting with folks at ConservAmerica, town and city revitalization committees, regional Chambers of Commerce, and the business community. We have so much invested in our waters. While pondering this, I scribbled some thoughts and turned it into this info-graphic (below). I like how it came out. Let me know what you think.

HWC_wordle3

Convergence: Where Streams & Stories Connect

Eighteen years ago, my brother and I eloped with our mother to Kaua’i. I say “eloped” because the trip was a romantic surprise after my step-dad proposed over the phone. He was already there—on Kaua’i. It was February, 1995, my senior year of high school, and the end of February school vacation. I turned 18 during the 23 hour plane ride to the Big Island of Hawai’i. My parents—my mother and step-dad, married at the point of convergence, where two streams met before emptying into the Pacific. Waterfalls peeled like tropical fruit through the rainforest. Two fed these streams. Neither my brother nor I had ever experienced swimming in the Pacific Ocean, let alone kayaking through a jungle. One day we hiked to a massive 40-foot waterfall, which we learned had been featured in one of the King Kong movies. I slipped behind the falls into a cave, sprayed by its awesome force. Those streams created our new family.

Flash forward to 2013:  A small perennial stream meanders through my black ash seep, past a vernal pool and flows into the pond. It’s not dramatic. It’s barely audible. The nor’easter that took everyone on the East coast by surprise yesterday dropped over a foot of snow. It’s that light fluffy stuff perfect for a snowshoe hike. Everything’s quiet, cold and white. Yet the stream trickles, melting the snow on either side. It persists. This stream is one of many, many streams in Maine that flow either perennially, intermittently or ephemerally—that is, after storms. Streams criss-cross and converge, form major tributaries like Panther Run, feed creeks and rivers, such as the Crooked River, emptying into lakes, picturesque waters such as Panther Pond, and wetlands throughout the Sebago Lakes Region of southern Maine. Most of the residents in this region depend on the groundwater for their drinking water. Those residents in the Portland Water District get their drinking water from Sebago Lake. Either way, the streams that flow and converge throughout the state—even beyond this watershed—play an integral part of life as we know it.

In thinking about the importance of headwater streams, it’s useful to see streams in a larger watershed context. The U.S. Environmental Protection Agency (EPA) has launched a great online tool with a headwater stream index for the entire United States. Maps showing stream data are available for 48 states (Alaska and Hawai’i are not available at the time of this post). EPA has published the summaries of findings from a 2009 study on intermittent, ephemeral and headwater streams. There’s information about public drinking water systems in the U.S., too. Local drinking waterinformation is also available by state.

What I found interesting in looking at stream data for the State of Maine is that I live in an area where 94-100% of stream miles are contained in Source Protection Areas (SPAs). An SPA is an area “upstream from a drinking water source or intake that contributes surface water flow to the drinking water intake within a 24-hour period.” (EPA, Office of Water) That means that most of, if not all of, the intermittent, headwater and ephemeral streams in those areas support public drinking water systems.

It makes sense. I live in a town that’s home to the “landlocked salmon” in Sebago Lake. The lake is one of the few lakes in the country that receives a Filtration Avoidance Waiver from the EPA. This waiver saves the communities in the region $125 million in construction and operation costs—since there is no need for a water treatment facility. I recently learned that if the Portland Water District had to invest in such a water treatment system, it would cost over $100 million. Currently, the cost-savings come from the convergence of headwater, intermittent and ephemeral streams throughout the Sebago Lakes Region watershed.  We also know that area wetlands are equally valuable for their ecological services, including flood attenuation and protecting water quality in those very streams. It is my hope as a local conservation official, and through volunteering with small watershed groups, like the Healthy Waters Coalition in the Sebago Lakes Region, we can inform and educate municipal decision-makers on the value of protecting headwater streams.

Meanwhile, the Maine Association of Wetland Scientists is holding its annual meeting on March 25th. This year’s meeting focuses on rivers and streams.

For further reading, check out these related blogs:

Streams Take Me By Surprise, by Travis Loop, EPA blog

Rivanna streams not safe for swimming and boating? Find out more on Thurs, March 21
Rivanna River Basin Commission (Charlottesville, VA)

Managing Municipal Stormwater: Protecting Water Quality, Streams and Communities
Penn State Extension Blog

Rivers, Streams, Water Falls, Food and More, by Bill Trussell, Fishing Through Life

For further information about streams, click here.

Pond Scum: The Good, the Bad, and the Sludgy

Globs of algae the size of human heads floated around like something out of a B-movie on MST3K. It was unnerving to bump into one of them. I can handle swimming with eels…but I find it creepy to swim with severed head-shaped algae clusters. When I arrived at my little local lakeside beach in southern Maine, I thought I was lucky because no one else was there in 90-degree heat. Then I realized the beach was vacant because of the algal bloom. An algal bloom is a concentration of cyanobacteria. Strange Wetlands covered types of algae blooms, including blue green algae, in an earlier post (2010).

In the Great Lakes region this summer, some communities are seeing algal blooms, including the Eastern parts of Lake Erie. Algal blooms turn the water a bright scummy green. Some of the vegetation washes ashore in clumps, deterring beach goers but not always causing beach closings.  However, NOAA has recently issued a prediction that western Lake Erie should see a lesser algal bloom this summer. This is good news.NOAA, partners predict mild harmful algal blooms for western Lake Erie this year. A presentation will be held on algal blooms and the “Lake Erie Dead Zone” by an aquatic biologist in Cleveland Heights on July 25th.  For more information about the Lake Erie Dead Zone, visit EPA’s webpage. But this year’s bloom on Lake Erie is likely to be only one tenth the size of the bloom that occurred last year.

Last year, Lake Erie’s harmful algal bloom was visible from space (2011). In fact last year’s algae blooms in the Great Lakes were touted as the ‘worst since the 1960s,’ something akin to the comics of “The Creature from the Black Lagoon.” The Natural Resources Defense Council presented analysis of Ohio beach closings and algal bloomsand on New York beaches for Lake Ontario and Lake Erie with monitoring data collected in 2011. Full report here.

What’s the issue this summer? Not all algae, or “pond scum,” is created equal. Some amount of algae is a normal part of the ecosystem but too much of the wrong types are harmful. A Great Lakes native algae called Spirogyra is thriving on the conditions caused by invasive zebra and quagga mussels. The result is a sludge-like mat of green algae that washes up on beaches along Lake Michigan and other lakes. Another green alga, Cladophora, increased because of the zebra mussels, and both types of algae wash ashore in thick mats, which rot, stink and harbor E. Coli, Salmonella and other pathogens. The stench from the beach muck is comparable to manure. See video, “All Washed Up: Lake Michigan’s Algae Challenge.” For a fact sheet on Harmful Algae Blooms & Muck: What’s the Difference (Michigan Sea Grant), click here. For more about the relationship between algae and zebra mussels, see Changes in the benthic algal community and nutrient limitation in Saginaw Bay, Lake Huron, during the invasion of the zebra mussel (report, 2002).

Another serious factor this summer is drought, which is occurring in a large part of the country. For instance in Wisconsin, the hot weather has caused harmful blue green algae blooms in Lake Winnebago and Tainter/Menomin lakes, where there is a history of blooms, but the harmful algae is also showing up in lakes where it previously did not occur. They are facing a similar problem to that in Lake Michigan with the zebra mussels and Cladophora, warned to be harmful to boaters and swimmers. The US Fish & Wildlife Service has found dead waterfowl, most likely killed by botulism, in Wisconsin lakes this year. For a past FWS report on waterfowl and botulism in the Wisconsin lakes, click here.

Algal blooms are probably not at the top of the list of issues concerning those keeping an eye on the Farm Bill developments—but this is one of the reasons why the Farm Bill’s Conservation Title is so crucial to the protection of wetlands and water resources—including the Great Lakes. See Farm Bill Conservation Programs Are ‘Essential for Great Lakes Restoration’

Restoring Lost Ecological Connections: Fish Ladders and Dam Removal

Growing up in midcoast Maine I was accustomed to celebrating the return of the alewives, an anadromous, or sea-run fish, each spring. Recently a project to restore the fish ladder for the alewives has neared completion in a stream at Damariscotta Mills. The Maine state legislature called for a fish passage in 1741, which led to the town finally building the fish ladder in 1807 to allow the alewives to return to Maine’s streams, ponds and lakes to spawn. The project to rebuild the old fish ladder began 200 years later in 2007 and has entered a final phase in 2012. One challenge for the restoration crew has been to make sure that the fish ladder was functional for the alewives each season. The running of the alewives just occurred in late May/early June.

Meanwhile, another river in Maine supports the run of alewives, salmon, sturgeon and other sea-run fish: the Penobscot, Maine’s largest river. A major component of a restoration project to restore critical habitat in Maine’s largest watershed is underway this week along the Penobscot River. The Great Works Dam on the lower part of the river is being removed this week. See a video of this dam removal (June 11, 2012). This is the culmination of a lot of planning over the past eight years on the part of federal, state and tribal governments, along with nonprofit and for-profit parties.  These have included the State of Maine, The Nature Conservancy, National Oceanic Atmospheric Administration, Penobscot Nation, Maine Audubon, Natural Resources Council of Maine, Trout Unlimited, American Rivers, Atlantic Salmon Federation and other partners. Together they form the Penobscot River Restoration Trust. This project began in 1999, but an essential agreement formed in 2004 laid the groundwork for the collaborative restoration efforts. This unprecedented agreement set out to accomplish these things:

  1. Restore self-sustaining populations of native sea-run fish, such as the endangered Atlantic salmon;
  2. Renew opportunities for the Penobscot Nation to exercise sustenance fishing rights;
  3. Create new opportunities for tourism, businesses and communities;
  4. Resolve long-standing disputes and avoid future uncertainties over the regulation of the river.

The agreement further laid out a plan to remove two dams on the lower part of the river, including the Great Works Dam removed this week, and to construct fish bypasses by a third dam and to improve fish passage at four other dams. In 2007, the Penobscot River Restoration Trust and the U.S. Fish and Wildlife Service announced the project, and added that it would have far-ranging benefits on the Gulf of Maine, protecting endangered species, migratory birds, as well as riverine and estuarine wetlands. It would also enhance recreational activities, such as paddling and fishing and watching wildlife.  The riverine habitat is home to osprey, kingfishers, otters and bald eagles. The project has been widely known as one of the most innovative river restoration projects in the nation.

Some members of the Penobscot River Restoration Trust have made comparisons to the 1999 dam removal on the Kennebec, which was among notable dam removal projects that set a trend throughout the country. The two rivers share some of the same ecological communities. Those involved with monitoring the Kennebec since 1999, have noted a return of more birds, namely osprey and bald eagles, due to the increased number of alewives present, a food source for the birds of prey. “It’s restoring some of the lost ecological connections in the river. First, we’ve seen the rebuilding of the herring run. And now we’ve seen the building of the eagle and osprey populations,” according toAndrew Goode of the Atlantic Salmon Federation.

The Penobscot River and its tributaries flow through the Maine North Woods to Penobscot Bay, in midcoast Maine. Scientists began collecting baseline data for monitoring wetlands, rare plants, invasive species, geomorphology, water quality, smolt telemetry (tagging and monitoring the actively migrating young salmon), tracking fish movements and fish communities, including sturgeon, salmon and other species, in 2009. See monitoring poster. For more information about the monitoring work with sturgeon,click here.

Dam removal, fish passage and river restoration projects are happening in other parts of the country, too. Trout Unlimited has recently blogged about the legacy of “Making rivers whole again” and what’s considered the largest dam removal project in the country is underway in the Olympic wilderness of Washington state. The Elwha Dam removal project began last fall to restore the Elwha River and ecosystem. It’s managed by theNational Park Service. A recent look at case-studies on dam removal and legislation in the U.S. from an energy perspective was provided in “Exploring the Reasons behind Dam Removal.” In addition, the Connecticut River has become the first National Blueway thanks to the efforts of over 40 local, state and federal government agency and nonprofit and for-profit coalition members. The designation will improve recreational opportunities for boating, canoeing, trail-building and conservation along the river in four states: CT, NH, MA and VT. The idea originated out of President Obama’s “America’s Great Outdoors” initiative. For a snapshot of other ideas in the Great Outdoors initiative, click here.

Updated: April 4, 2013: Blocked Migration: Fish Ladders On U.S. Dams Are Not Effective

Tar Sands, Pipeline Proposals & Wetlands

In preparing for a conservation commission meeting, I have been learning more about the tar sands crude oil pipelines and the potential impacts they have on water resources. Previously, I had heard about the tar sands and oil spill on the Kalamazoo River in Michigan in 2010 and the crude oil spill in Yellowstone in 2011 (MT), but I did not know much about tar sands extraction and transportation into North America. Lately there has been some press about a New England proposal for an Enbridge pipeline project. For example, I read a NWF blog post last month and came across a number of useful background documents on state, regional and national issues related to tar sands crude oil pipelines on the Natural Resources Council of Maine’s website. Also in April, the National Wildlife Federation published a report, “After the Marshall Spill: Oil Pipelines in the Great Lakes Region,” which assesses the regulatory issues involved in protecting wetlands and waters in the Great Lakes from similar disasters in the future.

Heating oil pipelineFrom local issues to national concerns:  The topic of tar sands crude oil pipeline proposals in my community of Maine is echoed throughout the New England region, and throughout the U.S. all the way to the Gulf of Mexico. In southern Maine, Sebago Lake, the source of drinking water for the city of Portland, Maine and surrounding towns, plays a prominent role in a number of environmental advocacy groups’ efforts to halt proposals for pumping tar sands through the state. The pipeline currently runs from South Portland, Maine through the Lakes Region towns, including Windham, where ASWM is headquartered, crossing Panther Run and the Crooked River, which feed Sebago Lake. This is just one small area of the longer pipeline, which would cross through many other watersheds throughout New England.

After I presented information at my local conservation commission meeting, I ran into a few neighbors and residents who commented on the issue of a tar sands pipeline proposal that could have an impact on Maine’s watersheds and natural resources.  One business owner said, “They’re still cleaning up the spill in Michigan! If that happened here, we’d be done.” Similar views have been expressed at town meetings, on PBS presentations(winter 2012) and at university informational sessions in southern Maine. The Natural Resources Council of Maine has an ongoing project informing citizens about the proposal and its potential impacts to Maine, as well as the Enbridge proposals for tar sands pipelines elsewhere in the country. For a fact sheet on Tar Sands, Keystone Pipeline Project in Maine (2012), click here.

Boreal Forest Before and AfterWhat are tar sands and where do they come from? Tar sands are a mixture of clay, sand, water and bitumen, a heavy black viscous oil.  The process extracts the bitumen from the other materials and requires other treatment before it can be refined.  It is so thick it requires dilution with additional hydrocarbons before it can be transported through pipelines when it can be later turned into conventional heating oil. This process of transporting it in pipelines has many potentially hazardous impacts to water and other natural resources in the event of a spill.  Once the tar sands crude oil is transported, the process of turning it into conventional oil is not cost-effective or ecologically sensible.  The process releases more than double the harmful greenhouse gasses than conventional heating oil does during production. (See Scientific American.) Currently, the bulk of the tar sands originate in Alberta, Canada—where large pools called tar pits have replaced wetlands. These tar pits are big enough to be seen from space. The most threatened habitat are Canada’s boreal forests, which is 1.3 billion acres of wetlands—among the largest in-tact wetland ecosystems on Earth. Unfortunately, most of the wastewater involved with the tar sands production ends up in streams and rivers throughout the boreal forest, contaminating the wetlands and threatening bird and wildlife habitat. For Alberta’s Government webpage on oil sands, click here.

Alberta Oil Sands MapAccording to mining company reports, 64% of the mining landscape is made up of peatlands. (See related study, “Oil sands mining and reclamation cause massive loss of peatland and stored carbon.”)  There’s some effort underway to restore the wetlands that have been affected by tar sands in Alberta. Oil Sands Wetlands Reclamation: Syncrude, Suncor Plan To Reconstruct Fens It’s unconventional wetland restoration on a large scale. Essentially they’re hoping to recreate a 50-hectare watershed, not just a wetland, for one project. That’s about 125 acres of wetlands and waters. The University of Waterloo’s department of geography and environmental management is involved with the watershed restoration planning. It’s been called a Tar Sands Wetlands Reclamation. However, some Canadian wetland scientists are doubtful that this will work to restore the wetlands.  They say, “Instead of bogs and fens, the industry will build hills topped by plantation forests and fill large man-made lakes with toxic waste bordered by shrubs and salty marshes.” (Rooney, et.al., 2011)

“It’s a completely different landscape,” says study co-author Suzanne Bayley, one of Canada’s top wetland ecologists and a University of Alberta professor. See Scientists Doubt Fix to Wetlands Damaged by Oil Sands Furthermore, fewer wetlands means drier conditions and more fire hazards. See a related presentation on The State of Oil Sands Wetlands Reclamation and Slow Down Oil Sands to Save Wetlands, Scientist Says –with details from a related study of Canadian wetlands. For an Alberta wetlands fact sheet by Water Matters, click here.

So what about tar sands pipelines in the U.S.? In addition to the discussions ongoing in New England, there’s a lot of information available on the potential impacts and environmental risks of tar sands pipeline projects nationally. See Tar Sands Pipelines Safety Risks

By Natural Resources Defense Council, National Wildlife Federation, et.al. – February 2011

Tar Sands Invasion: How Dirty and Expensive Oil from Canada Threatens America’s New Energy Economy By NRDC, Earth Works, Sierra Club, et. al. – May 2010.

Further reading:

Study Disputes Oil Sands ‘Restoration’ Pledge (NY Times Green Blog, March 2012)
Tran-Canada’s New Permit Still Threatens Nebraska’s Water and U.S. Energy Security 
New Keystone XL Tar Sands Pipeline Permit Rejected by Nebraska Residents
 
In through the backdoor: Is Enbridge Inc. trying to bring tar sands to Central Canada and New England?

Sulfide Mining Regulation in the Great Lakes Region
 (includes links to series of reports on impacts to water resources in several states –WI, MI, MN, plus Ontario)
Cattle Ranchers, Environmentalists and the Keystone XL Pipeline

Video: Robert Redford and Waterkeeper Alliance on XL Keystone Pipeline Protest
 (2011)
May 2012 Update: The Great Lakes, New Dumping Ground for Tar Sands Oil
http://ecowatch.org/2012/the-great-lakes-new-dumping-ground-for-tar-sands-oil/

Destiny of Waters

Is it a lake or a pond or a wetland?

Recently someone asked me about the body of water beyond my backyard—if it was a lake or a pond and what’s the difference? My first answer was that it is a pond by name. A pond or lake may be named as such the way “street,” “lane,” or “road” are often interchangeable. Secondly, a lake and a pond have differences at the ecological level—in terms of aquatic life, and in terms of limnology.  I also explained that the differences had to do with acreage and depth of the water body. Sometimes a “pond” can be bigger and deeper by comparison to a nearby lake, as in the case of Long Pond (113’ deep) and Echo Lake (66’ deep) in Acadia National Park. In that case, Echo Lake is technically considered a “great pond” under Maine state law because it’s a natural pond greater than 10 acres.  But usually lakes are bigger and deeper than ponds. State definitions generally include both lakes and natural ponds as “waters of the state.” Under the Cowardin classification system, ponds are wetlands.

What I did not explain to my friend very well was the natural gradation of lakes into ponds into wetlands, and their evolution as waters.  What made sense to me as an ecologist, that one type would naturally grade into another water type, was harder to explain. What’s even harder to illustrate is the concept of an ecotone—the transitional area between two ecological communities adjacent to one another. As usual, I thought of movies.

The phenomenon of distinct communities existing side by side can be observed in film.  For example, the liminal space between cultures—a cultural transition area—can be viewed as bordercrossings, illustrated effectively in films like “Night on Earth” (1991). Jim Jarmusch’s film took place entirely in taxi cabs in five different time zones throughout the world. The concept is that no matter where you go, at one point in time, there are eerily similar transactions and interactions taking place in taxi cabs—a kind of cultural habitat, if you will—for humans migrating from one place to another. Some water bodies, like taxi cabs, are mobile; some are stationary, like an ‘off-duty’ cab.  And that’s where the changes from lake to pond to wetland, or the line between adjacent ecological communities, can get a little fuzzy to someone standing on the curb, er, the edge of the water.

Over what period of time do lakes become ponds? How long does it take for ponds to become wetlands? For wetlands to become meadows? The short answer is several thousand years, if nothing has interrupted (or accelerated) the natural evolution of these waters. This is called succession. Biology students learning about wetland succession in a classroom can experiment with an aquarium—starting with a mini pond or wetland habitat. For a biology teaching guide written by BioMedia (Russell) that outlines the key ingredients to such an experiment for a year-long study,click here. Limnologists say, “lakes are destined to die,” whereas ponds are the “death of a lake” and the “birth of a marsh.” For an explanation on pond succession, click here.

So how does a pond become a wetland? The first stage, called the ‘pioneer’ stage of wetland succession, starts with the pond without plant life at the bottom. Plankton, which inhabit the pond, and carry miniscule plant and animal life, arrive on the winds or wings of insects.  Over time, plankton die on the pond bottom and create a mucky layer, which is rich enough for water emergent plants to grow, such as water lilies, ancient wetland plants. As water lilies form a blanket over the surface of the water, they cut off the sunlight to the bottom, killing off the submergent plants. These processes can take a variety of timeframes from a matter of years to a matter of millennia. Trees, shrubs and grasses move into the space that was once the pond and a wetland takes shape. This is a dynamic process with many variables. Some wetland ecologists have argued against the idea of wetland succession because of these variables.

Succession is not a sure thing. It does not occur with all lakes in the U.S.. (For instance, there is no scientific concern that the Great Lakes will eventually turn into ponds, or meadows.) There are many factors that can interrupt a “natural” succession process such as a changing climate, soils, drainage, land development, introduction of invasive plants or other aquatic species, phosphorus run-off (causing dissolved oxygen) or other factors.

In addition to the possible succession pattern of pond to wetland, some wetlands can be turned into ponds. In the U.S. Fish & Wildlife Service’s Status & Trends of Wetlands in the Conterminous United States 2004-2009, ponds are recognized as a type of freshwater wetland. The report indicates a net increase of 207,200 acres of ponds between 2004-2009, an increase of 3.2% in ponds nationally (FWS).  The trouble with ponds, for example, farm ponds, being created while another type of freshwater wetland is lost, is that there is a difference between constructed ponds and wetlands—including natural ponds, in terms of their ecological functions. According to the Status & Trends Report, the majority of ponds in the U.S. are constructed farm ponds. Only 31% of the ponds in the lower 48 states are natural.

Mankind has a dramatic impact on natural landscapes frequently disrupting succession. This means it’s an uncertain destiny for our lakes, ponds, streams, rivers and wetlands. For those working to protect wetlands, and to harness the power of wetlands to sequester carbon and provide unique and solvent ways to fight climate change’s impact on our planet, this is cause for concern. Save wetlands, save ourselves.

Helpful Resources:

Massachusetts Lake and Pond Guide

Wisconsin’s Natural Communities

Michigan DNR: Succession – Changing Land, Changing Wildlife

Wetland Ecosystems by William J. Mitsch, James G. Gosselink et. al. (2009)

Wetland Ecology: Principles and Conservation, 2nd Edition by Paul Keddy, (2010)

ASWM’s Wetland Science web resources

Other recent blogs on wetland succession:

Conservation Maven: Study finds post-restoration wetland succession highly variable

Ian Lunt’s Ecological Research Site: There’s a wetland in my grassland

Constantine Alexander’s blog: Artificial wetlands can provide benefits over the long haul(on Bill Mitsch’s work on wetland creation and succession)