Category Archives: Conservation & Restoration

Glaciers as Social Spaces: Oral Histories, Frankenstein, and Pearl Jam’s Gigaton

Lately I’ve been thinking about glaciers. I re-watched “Chasing Ice,” which is a fascinating documentary film with the first large-scale ground survey of glaciers, directed by Jeff Orlowski and led by photographer James Balog. I’m sure you’ve seen Balog’s incredible documentary films on PBS/NOVA if not “Chasing Ice” or his photography in National Geographic.

Thinking of glaciers as “social spaces” allows us to consider the effects of climate change on the cryosphere—the frozen layers of the Earth, including glaciers and permafrost, from a variety of perspectives. We can examine glaciers as “social spaces” by exploring the ethnography of oral history traditions in the Yukon Territory, the socio-economic impacts, such as the melting of the cryosphere, in those ‘social spaces’ in Alaska, as another example. Additionally, we can explore glaciers as social spaces in literary ecology and contemporary music. How do glaciers “listen?” I explore a few ways below.

51Z+K0PRVIL._SX332_BO1,204,203,200_The senior women of the Saint Elias Mountain region of the southern Yukon Territory (Canada) relayed complex natural and social histories to anthropologist Julie Cruikshank when she did ethnographic research recording the life stories of Athapaskan and Tlingit elders. Her book, Do Glaciers Listen?: Local Knowledge, Colonial Encounters, and Social Imagination was published in 2005 (Paperback edition, 2010) but I think it’s still highly relevant. She found that the elders, “grounded precise social histories of twentieth-century life within a scaffolding of much older narratives. [They drew] on established long narrative conventions to reflect on complex life circumstances. In the words [of one elder] Angela Sidney, ancient narratives had helped her to ‘live life like a story.’” (Cruikshank, 2005) Cruikshank, while living with the elders, “heard narratives about glacial caves inhabited by intemperate beings that might emerge unexpectedly: and others that depicted glaciers as living and responsive themselves. Stories dramatized […] bursting of ice-dammed lakes into river valleys, and […] told stories of travel […] sometimes crossing crevasse-ridden glaciers on foot and sometimes piloting hand-hewn cottonwood boats beneath glacial bridges…” (Cruikshank, 2005) They told stories of strangers called “cloud people.” (Cruikshank, 2005) The women’s stories depicted a “winter world” that crossed economic borders, of coastal Tlingit traders, and the shifting power relations described by economic historian Howard Innis on the 19th century market for furs, gold, cod and timber. (Cruikshank, 2005) Cruikshank’s writing is wonderfully evocative of the culture and arctic wonder.

Glaciers, according to the stories, radiate heat and energy. They’re alive. Cruikshank pores into the Athapaskan elders’ stories like a glaciologist drills an ice core, studying its layers, noting the environmental, geophysical changes in a glacier—which tells a social story, since glaciers are part of the Athapaskan and Tlingit life stories. The Little Ice Age (1550-1850) is within reach of the memories of Athapaskan and Tlingit elders; some of their stories are memory and some, myth. After the Little Ice Age, the glaciers receded enough to make coastal lands accessible to Eyak, Tlingit, and Athapaskan nations to converge. Stories map the geography and human ecology of the glaciers and the ecological and social corridors connecting glaciers. Through the study of oral histories, we can glean that “glaciers present some navigational, spiritual, and intellectual challenges of a sentient “land that listens.” (Cruikshank, 2005) This is what is known as sentient ecology. (Ingold, 2000) This is what the elders explained to Cruikshank when they told her stories about glaciers listening and responding.

Similarly, a human ecologist could study the environmental changes, such as those impacts from global climate change on glaciers and permafrost, two related ecosystems, and their ecological place in our world—both as social spaces and quintessential geophysical, temporal yardsticks with which we measure global environmental change. These stories, from oral tradition, captured local traditional knowledge of the Saint Elias Mountain region of southern Yukon, and other parts of Canada, and the stories themselves seemed to shift and transform infinitesimally much like the glaciers.  One of the elders, Annie Ned, told stories of “caribou ‘blackening the ice’ on nearby lakes early in the (20th) century.” (Cruikshank, 2005) When Cruikshank and Shelia Greer prepared a report on the region’s oral history for the Archaeological Survey of Canada, Ned’s story about the caribou became important in another context: “Scientists reporting discoveries of ancient tools and caribou droppings melting from a high alpine ice patch above [Ned’s] trapline cited her oral account in their initial scientific paper on prehistoric caribou.” (Cruikshank, 2005) Thus, the oral histories were not solely cultural translations and transcriptions of the women’s life stories; the stories were also part of a larger natural history of the region. Also, the issue of personhood comes into play: these women tell stories that “summon up a moral system that includes relationships with non-humans – animals and also features of the landscape, like glaciers – that share characteristics of personhood.” (Cruikshank, 2005) I am intrigued by the idea of personhood, the Rights of Nature movement, and an old idea—perhaps ancient, and pan-human, of connecting with land and water—the way headwater streams braid and combine to form a stream, intermittent or ephemeral—after storms, and each stream tells a story as it carves through sediment in the streambed. Similarly, anthropologists and human ecologists study the layers of permafrost, or analyze the many ways to tell a story about navigating a crevice in a glacier—the successful and failed rescue attempts, in order to discover the human dimensions of that glacial ecology. Literary ecologists seek to find meaning in the stories of the ways in which people interact with the natural world, including glaciers.

In Mary Shelley’s novel, Frankenstein (1818), she begins and ends the famous story about the mad-scientist, Victor Frankenstein, a graduate student from Geneva, and his creation, a Monster, comprised of human parts reanimated by electricity—on a glacier in the Arctic. At the start of the novel, a ship captain writes to his sister about encountering a strange man, crossing the ice on a sled, totally bereft but driven by a vengeance to confront his creation, the Monster, who fled to the “Land of Mist and Snow,” the glacial Alps, because he wanted a refuge from the cruelty of mankind. At the end of the novel, the reader rejoins Victor and the Monster, as they have one final showdown on the glacier. In Shelley’s real life, she and her fiancé Percy B. Shelley, had traveled through the region of Mont Blanc, home to Mer de Glace, the second largest glacier in the Alps in 1816. Later, while pregnant, Shelley writes the novel, the plot of which takes her heroes to Mer de Glace, that glacier. “Until the eighteenth century, the Alps were believed to be infested with devils, monsters and dragons. By setting her story of Victor Frankenstein and his Monster at Mer de Glace, Shelley links Victor’s activities with those of mountaineering scientists like Horace Benedict de Sausure.” (Nardin, 2006) Why set a story on a glacier? Her 19th century readers most likely shared her interest in alpine mountaineering, science and exploration. (Mary Shelley was an explorer herself; she had the moon in Sagittarius, a sign associated with wide open spaces, exploration of great frontiers and the outdoors. She was well-traveled even before she met Percy, and then they traveled Europe together. The astrological piece is my own theory.) In their travels, Percy and Mary stopped at inns along the way, and heard German stories, including a strange tale about a 17th century alchemist who had lived at Frankenstein Castle. (Sampson, 2018)

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In studying Romanticism, and in particular the work of Mary Shelley, I would argue that she pushed the borders of what it meant to be human, and the limits of our imagination surrounding consciousness and creation. Her two heroes, the Monster and his creator, Victor, are both intellectual, Miltonic philosophers; the epistolary structure of the novel has several characters communicate via letters; but the Monster, by contrast, writes in a journal. After failed attempts to socialize, he took refuge in the forest, along the river, and in the Alps at Mer de Glace. At Mont Blanc, he built himself a house, an ice cave within the glacier, and that became his home. He desired a mate and implored Victor to supply him a female counterpart, who the Monster planned to live out his (immortal) days, at Mont Blanc on Mer de Glace. I wish I had a cool photo of Mer de Glace–but I haven’t traveled there–but a quick Google Images search yields lots of incredible photo results! Have you been there? Leave a comment and let me know what it was like!

I am currently reading Mary Shelley’s travel journal, which includes her experiences traveling through the Mer de Glace area (I think she and Percy saw it from a distance). Screen Shot 2020-03-11 at 9.34.13 PM

Last year, I began to analyze Shelley’s use of water and wetland metaphors throughout her novel as part of my graduate work in literary ecology. It’s intriguing that she creates this social space on the glacier—instead of within a city, or along a river, or in a forest—other places where the Monster hides and takes refuge throughout the story. The Monster feels safe in the harsh environs of the glacier. Unlike a man, the Monster is not vulnerable to the cold, strong winds, snow and ice. Other scholars, researchers, poets and writers have shared this fascination with Shelley’s use of the glacier, Mer de Glace, as a social space in Frankenstein. I am analyzing this as a part of my literary ecology of works by Romantic women writers–and still have a long way to go to read and digest what scholars have already discovered.

I wrote a Mary Shelley tribute poem, “The Bride of Frankenstein’s Monster, On the Eve of Her Wedding,” published last summer on Boned literary magazine’s site; my poem revisited the idea of the Monster, having his wish granted for a mate, and is about to return to the glacier. I wrote the poem from her perspective, while she is preparing for a life in the “Land of Mist and Snow.” This is one way that I have explored Shelley’s novel from an ecofeminist perspective.  For the bicentenary of Frankenstein, poet and scholar Fiona Sampson published the biography, In Search of Mary Shelley: the Girl Who Wrote Frankenstein (2018). I loved this biography!! She writes, “Mary has ‘gone missing’ from literary history; she has faded to white like Frankenstein’s creature who ‘goes out, alone again, onto the Arctic ice to die.’” (Hewett, 2018) The iconic profile of the Monster, loping out across the ice, has haunted my imagination since I first read Frankenstein at seventeen, while my family lived in a historic, haunted house in Maine.

I have been having fun playing with this “Literary Witches” deck of cards, by Katy Horan and Taisia Kitaiskaia, who created a clever way of translating mini biographies on each card of women writers from all sorts of genres and all sorts of periods of literature–from all over the world. Perfect activity for International Women’s Day and Women’s History Month! I like to use the cards for inspiration. And yes, Mary Shelley is in this cute deck. The idea is that each of these writers created “magic” through their literary works. (None are suggested to have been “witches” here–it’s just a clever metaphor.)

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Part of Shelley’s genius was her way of weaving together Enlightenment and Romanticism-era science, the including the invention of electricity and the Linnaean classification system, her mother, Mary Wollstonecraft’s botany and natural history articles, as well as Shelley’s own explorations with Percy, sometimes with a toddler in tow, endowed her with additional “tools” of her trade. Her novel brought glaciers to life for readers with her first-hand observations; she enlivened Mer de Glace into an imaginary landscape accessible to her readers. Today’s literary ecologists are re-examining works in Romanticism (and later periods) to extrapolate Romantic ecology, “dark ecology” and the EcoGothic—related themes that frame how we continue to think about the environment today. Industrialization occurred at the time when Romantic ecology was born—the onset, as many scholars believe, of the modern environmental movement. Is it still relevant? There are some literary ecologists who believe we are still in a Romantic treatment of nature. Paul Kingsnorth and Tim Morton, two ecology writers who promote the idea of a “dark ecology,” are examples of those who believe the age of Romantic ecology may never have ended. We continue to be awed by glaciers—their melting, their sublime power, even, on a smaller scale, glacial erratics—geologic memories of prehistoric, ancient glaciers.

In socio-economic terms, we can analyze the social space of a glacier, and related ecosystems, such as permafrost, and the effects of climate change on that ‘social space,’ for instance, in Alaska, where communities have already been seeing socio-economic impacts of climate change. These impacts include the need for relocating and replacing infrastructure that’s been damaged, lost or threatened by permafrost thawing. Permafrost is a frozen, arctic wetland type; specific grasses, lichens and shrubs are frozen in water most of the year, in some places, frozen year-round (thus the name permafrost) creating a carpet-like vegetation. Thinning, melting permafrost can be found at Wrangell-St Elias National Park and Preserve in south central Alaska. Glacial melting has caused increased large landslides in the national park. In 2015, 180 million tons of loose rock fell into the Taan Fjord causing a huge tsunami-like swell that flattened forests. “Tsunamis of some sort triggered by landslides in bays or lakes are fairly common, but it’s rare that they’re this extreme,” according to Brentwood Higman, author of a study on tsunamis in the Taan Fjord, Alaska. (2018) Melting permafrost is also allowing archaeologists ways of uncovering evidence of human and animal use of the cryosphere—with brown ice layers revealing evidence of caribou use, such as illustrated by the senior women of the Saint Elias Mountain region whose stories Cruikshank recorded and transcribed—detailing their ancestral memories of the “browning ice” phenomenon associated with caribou use. Additionally, archaeology of melting glaciers provides newer access to human artifacts such as wood arrow shafts, darts made of antlers, and birch bark basket fragments found in Wrangell-St. Elias National Park and Preserve. (Dixon, et al. 2005) This is, I think, further evidence of the value of oral histories in adding historic context and narrative basis behind newer findings during archaeological research projects made possible in part by glacial melting and permafrost thinning in that region.

In a 2018 study on the economic effects of climate change in Alaska—pertaining to changes to glacial ecology, including permafrost melting, “five certain large effects can be quantified, […] to impose an annual net cost of $340-700 million of Alaska’s GDP.” (Berman and Schmidt, 2019) These large effects include the melting and thawing of the cryosphere—notably glaciers and permafrost. “Glacial melt affects availability of phosphorus, iron and organic carbon to terrestrial and marine organisms.” (Berman and Schmidt, 2019) “Melting glaciers will increase the role of seasonal precipitation patterns in determining hydroelectric capacity.” (Berman and Schmidt, 2019) The melting of the cryosphere affects several industries in Alaska and ‘social spaces’ including fishing, forestry, energy demand, tourism and recreation, agriculture, marine and coastal shipping, as well as public infrastructure. (Berman and Schmidt, 2019) For native Alaskans, the effects of climate change on the cryosphere include impacts to subsistence living:  “harvest cycles, changes in important food sources, loss of some locations used for fishing and waterfowl hunting,” are among the changes affecting those social spaces. (Berman and Schmidt, 2019) The largest effects are directly caused by melting glaciers and permafrost in western and northern Alaska. (Berman and Schmidt, 2019) There are far more examples, but these are just two significant ones that quantify the effects of climate change on the cryosphere—and that as a “social space.”

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Glaciers are weighed in gigatons. Pearl Jam, my soul (read: more than favorite, since 1992) band, is an environmental activist band. Pearl Jam’s new album, Gigaton, features the close-up image of a glacier on its cover, (at left) and while it’s not out yet, I will be surprised if there isn’t a song about glaciers, or something environmentally-conscious. (I will post a review once the album comes out March 27th.) I love their new song from this album, “Dance of the Clairvoyants.” Pearl Jam has, in the past, taken inspiration from environmental issues like coastal wetlands, hurricanes, and ocean conservation and incorporated those into their music and activism. They create a social space for environmental activism through their music, their Surfrider Foundation, and their concerts. That’s another way of exploring a glacier as a social space. Set it to music.

Berman, Matthew and Jennifer Schmidt. “Economic Effects of Climate Change in Alaska.” Weather, Climate and Society. April 2019

Cruikshank, Julie. Constructing Life Stories:  Glaciers as Social Spaces, from Do Glaciers Listen?: Local Knowledge, Colonial Encounters, and Social Imagination. 2005

Dixon, E. James, William Manley and Craig Lee. “The emerging archaeology of glaciers and ice patches: examples from Alaska’s Wrangell-St. Elias National Park and Preserve.” American Antiquity. Vol. 70, Issue 1. Jan. 2005

Hewett, Rachel. “In Search of Mary Shelley Fiona Sampson Review.” The Guardian. Jan 2018

Ingold, Tim. The Perception on the Environment: Essays on livelihood, dwelling and skill. 2000

“Mountain Waves: Glacial melt is increasing land instability in mountainous regions, with huge tsunamis rising in frequency as a result.” Geographical. Vol. 90, Issue 11. Nov. 2018

Nardin, Jane. “A Meeting on Mer de Glace: Frankenstein and the History of Alpine Mountaineering.” Women’s Writing. Vol. 6. 1999

Sampson, Fiona. In Search of Mary Shelley: The Girl Who Wrote Frankenstein. 2018

Rarity and Ocean Conservation: Endangered Sawfish, Final Listing on ESA

On 8th Grade “Career Day,” my classmates and I were asked what we wanted to be when we grew up. I remember looking at a giant phonebook-sized directory of “careers” with code-keys for filling out a handout in class. I chose “marine biologist,” “oceanographer,” and asked my teacher, “where’s the code for “Ichthyologist?” Admittedly, I also wanted to write down on my sheet that I

Rachel Carson, marine biologist, author of The Edge of the Sea, Under the Sea Wind, and Silent Spring. Alfred Eisenstaedt photo, Time Life Picture

Rachel Carson, marine biologist, author of The Edge of the Sea, Under the Sea Wind, and Silent Spring. Alfred Eisenstaedt photo, Time Life Picture

considered “mime” and “poet” to be future, possible careers, but only one of those was true. Poetry remains a constant passion for me, and so does ocean conservation. I grew up reading poems by Edna St. Vincent Millay and essays by Rachel Carson, including her book, A Sense of Wonder and later in high school, The Edge of the Sea, which remains one of my favorite books of all time. In 9th grade, I bought a text book on marine biology with babysitting money and studied it outside of school, over the summer, while I studied biology at Gould Academy. Years later, at College of the Atlantic (COA), I studied conservation biology, island ecology and environmental sciences as an undergraduate student. During a summer field course, my COA classmates and I explored over 30 Maine islands and visited Gran Manan, where we saw a 30-foot basking shark in the Bay of Fundy. Studying at COA, usually in a salt-sprayed hammock overlooking the ocean, definitely helped to shape my early passion for islands, oceans and wetlands into a career in conservation.

Sharks, rays and sawfish have always been fascinating to me. (Ocean conservation nerd alert: I even have a notepad from the American Elasmobranch Society on my desk.) I’ve spent some significant time on wetlands in my career, but I’ve also followed ocean conservation with great interest, never leaning too far away from my coastal roots. One area of ocean conservation that has kept my interest over the last two decades has been rare and endangered marine species, such as sawfish, which is the first sea fish to be listed on the U.S. Endangered Species list.  In recent years, there’s been some hope for sawfish populations in South Florida (see this video). Yet, rules published by the National Marine Fisheries Service listed five species of sawfish as endangered this past month in its final ruling.

Smalltooth sawfish. NOAA image

Smalltooth sawfish. NOAA image

“The final rule contains the Service’s determination that the narrow sawfish (Anoxypristis cuspidate), dwarf sawfish (Pristis clavata), largetooth sawfish (collectively, Pristis pristis), green sawfish (Pristis zijsron) and the non-U.S. distinct population segment (DPS) of smalltooth sawfish (Pristis pectinata) are endangered species under the ESA.” (Miller, December 2014)  (See info on the rule in the Federal Register here.)

What makes a thing like the sawfish rare?

Rarity is driven by scale—how many, how much, how big an area. Rarity means that something occurs infrequently, either in the form of endemism, being restricted to a certain place, or by the smallness of a population. In conservation biology the proportion or percentage of habitable sites or areas in which a particular species is present determines the rarity of a species.[1] In addition to the areas in which a particular species is present, the number of individuals found in that area also determines its rarity. There are different types of rarity which can be based on three factors: 1) geographical range – the species may occur in sufficient numbers but only live in a particular place, for example, an island; 2) the habitat specificity – if the species is a “specialist,” meaning it might be confined to a certain type of habitat, it could be found all over the world but only in that specific habitat, for example, tropical rainforests; 3) the population size – a small or declining population might cause rarity. [2] Generally a species can be locally very common but globally very uncommon, thereby making it rare and furthermore, valuable. A species can also be the opposite, globally common but spread out few and far between so that individuals have a hard time sustaining their populations through reproduction and dispersal.

But usually when a person thinks of rarity, they are probably thinking about a species that occurs in very low numbers and lives in only one place, as in many of the endemic creatures on the Galapagos Islands. It is this latter-most perception of rarity that plays a critical role in conservation work. People value rarity because it makes a living thing special—even if it had intrinsic value before it became rare, if it ever lived in greater numbers or more widespread populations.

Sawfish illustration by NOAA

Sawfish illustration by NOAA

Sawfish are a rare, unique—and critically endangered group of elasmobranches—sharks, skates and rays, that are most known for their toothed rostrum. Once common inhabitants of coastal, estuarine areas and rivers throughout the tropics, sawfish populations have been decimated by decades of fishing and survive—barely—in isolated habitats, according to the Mote Marine Laboratory in Florida. Seven recognized species of sawfish, including the smalltooth sawfish (Pristis pectinata), are listed as critically endangered by the World Conservation Union. In addition to the extensive gillnetting and trawling, sawfish are threatened by habitat degradation from coastal development. Sawfish prefer mangroves and other estuarine wetlands. Currently the sawfish population is believed to be restricted to remote areas of southwest Florida, particularly in the Everglades and the Keys. Sawfish are primarily a freshwater-loving creature but they occasionally go out to sea. Lobbyists proposed to add sawfish to Appendix 1 of CITES in 1994 (as part of the first Shark Resolution) to stop the trade in saws but the proposal was defeated in 1997 because it could not demonstrate that stopping trade would provide the necessary protection in wild populations. [See Petition to List North American Populations of Sawfish, 1999, here.] Subsequent proposals in 2007 and 2013 were successful, according to Shark Advocates International. According to the Mote Marine Laboratory conservation biologists, “even if effective conservation plans can be implemented it will take sawfish populations decades, or possibly even centuries, to recover to post-decline levels.” This is the fundamental crux of rarity in conservation biology: even if we do perfect conservation work, once a species is rare and critically endangered, it can take much longer for a species to recover than the time it took to reach the brink of extinction.  In November 2014, all sawfish species were listed on Appendix I & II of the Convention on Migratory Species (CMS).

Sonja Fordham of Shark Advocates explains to me:  The listing of smalltooth sawfish is therefore the most relevant; it has resulted in critical habitat designation, a comprehensive recovery plan, cutting edge research, and encouraging signs of population stabilization and growth.

See this NOAA Fisheries video on smalltooth sawfish conservation.

Several different organizations, in addition to federal and state agencies, are working to protect and conserve sawfish habitat and the endangered species. Here are some links to a few of these organizations and their fact sheets on sawfish:

Save the Sawfish

Sawfish Conservation Society

Shark Advocates, Fact Sheet on Smalltooth Sawfish

Florida Museum of Natural History, Sawfish Conservation

Save our Seas, Conservation of Sawfish Project

Fact sheet for the 11th Meeting of the Conference of the Parties (CoP11) to the Convention on Migratory Species (CMS) on Sawfish (5 species)

IUCN Global Sawfish Conservation Strategy 

[1] Begon, Michael, John L. Harper, Colin Townsend. Ecology: Individuals, Populations, and Communities. Blackwell Scientific Publications, Oxford, London, et. al. 1990. Glossary pp. 859..

[2] Pullin, Andrew. Conservation Biology. Cambridge University Press, 2002. pp.199-201.

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

The State(s) of Sea Level Rise Science

Peaks Island, Maine

Peaks Island, Maine

In early April, I read an issue of a Peaks Island, Maine newspaper. On the front page, a story’s headline caught my eye:  “Sea level rise not caused by climate change, scientists confirm.” At first I assumed it was an April Fool’s joke, but the date was not April 1st. Then I got upset. I read. It seems that the journalist had (mis)interpreted a report on sea levels in Casco Bay that affirmed the sea level has risen for much longer than most people have known about global climate change. In fact, the State of Maine has over 100 years worth of sea level rise data because the City of Portland has tracked sea level in Portland harbor since 1901. That’s valuable data. The University of Southern Maine has conducted a series of studies on sea level rise, sustainability and the economics involved with planning for adaptation. According to the Environmental Finance Center at the Muskie School (USM), “at least 100 coastal New England towns will be impacted by sea level rise and increased storm surge from climate change.” Read about their COAST and Climate Ready Estuary projects here.

The State of Maine published its climate change action plan in 2004. It identified sea level rise adaptation planning as a necessity. In particular, the Maine Geological Survey conducted several pilot projects that assessed coastal wetland migration. The state’s coastal zoning laws and management practices changed several years ago to reflect sea level rise. Read the 2010 report, “People and Nature: Adapting to a Changing Climate, Charting Maine’s Course.” A great list of collaborators contributed to the development of “People and Nature,” including Natural Resources Council of Maine, several state agencies, several cities and Maine Coast Heritage Trust. It’s hard to find on the state’s website because the State Planning Office’s website was moved and merged with those of other departments.

Meanwhile, adaptation planning has moved to the forefront of climate change science in recent years. Sea level rise scientists at NASA, USGS and other agencies engaged in an online chat session about the state of the science for sea level rise and adaptation planning in early April 2013. (You can listen to the discussion after-the-fact.) What I found interesting is that salt marsh ecology and wetlands play such a vital role in our understanding of sea level rise and its implications for coastal systems. Over the past 6 years, I’ve done some research on sea level rise and learned of sea level rise tools and adaptation planning efforts underway all over the country. A hotspot for sea level rise research is the East coast of the United States, where sea level rise is occurring at a faster rate between Cape Cod and the coast of North Carolina—faster than anywhere else in the world.

Leah Stetson photo

Leah Stetson photo

Several other states have begun to plan for sea level rise. Click on the links below to learn more about what states are doing about sea level rise and adapting natural resource management strategies for climate change. In most cases, it’s a collaborative effort.

MA: Mass Fish & Game Adaptation Planning       MA sea level rise planning maps
MA: Climate Change Adaptation Advisory Committee
NY: New York Sea Level Rise Planning        NY Sea Level Rise Task Force Report 2010
CT: Connecticut Climate Change Adaptation Reports
RI: Rhode Island Coastal Resources Management Council Sea Level Rise Planning
NJ: New Jersey Coastal Management Program Sea Level Rise Planning
NJ: Sea Level Rise in New Jersey, New Jersey Geological Survey Report, 1998
NJ, DE, PA, NY: Delaware River Basin Commission Climate Change Hydrology Report, 2013
DE: Delaware Sea Level Rise Planning & Adaptation
MD: Living Shorelines Program (Chesapeake Bay Trust)
MD: A Sea Level Response Strategy for Maryland (2000)
VA: Planning for Sea Level Rise, Virginia Institute for Marine Science
VA Sea Level Rise Maps
VA: Sea Level Rise Planning at Local Government Level in Virginia
VA: Government Plan for Development of Land Vulnerable to Sea Level Rise
GA: University of Georgia, Sea Grant – Sea Level Rise Planning & Research
FL: Florida’s Resilient Coasts: State Policy Framework for Adaptation (PDF)
FL: Multidisciplinary Review of Current Sea Level Rise Research in Florida  (University of Florida)
MS & AL: Mississippi and Alabama Sea Grant Consortium – Resilience in Coastal Communities
Gulf of Mexico States: Climate Community of Practice: Sea Level Rise Planning
LA: Coastal Protection & Restoration – Recommendations for Sea Level Rise Planning (Includes Louisiana’s 2012 Coastal Master Plan)
CA: California’s Climate Change Adaptation Plan for Water Resources (2012)
CA: State Resources on Sea Level Rise and Adaptation Planning
CA: Adapting to Sea Level Rise Report (2012)
CA, OR, WA: Sea-Level Rise for the Coasts of California, Oregon and Washington (2012)
OR: A Strategy for Adapting to Impacts of Climate Change on the Oregon Coast (2009)
OR: LiDAR Sea Level Rise Research (NOAA Digital Services)
WA: Addressing Sea Level Rise in Shoreline Master Programs (Guidance) (2007)
WA: Sea Level Rise Assessment: Impacts of Climate Change on the Coast (2007)
AK: Alaska’s Melting Permafrost and Melting Sea Ice (national research)
AK: Climate change impacts in Alaska (EPA)
NC: North Carolina Coastal Federation – Sea Level Rise

A note about North Carolina: Several state agencies, including the Departments of Environment & Natural Resources, Transportation and Commerce, all identified threats and risks from sea level rise in 2010. At the time, the state’s Governor signed a letter confirming this. Two years later, North Carolina’s State Senate passed a law that banned sea level rise adaptation planning based on the current science. The House of Representatives rejected the bill, but a compromised version of the bill called for a new study on sea level rise for North Carolina and a ban on exponential sea level rise predictions in modeling. Read this Scientific American article on NC and sea level rise, and the 2012 USGS study that found increasing sea level rise impacts on the coast between Cape Cod and the Carolinas. See “More unwanted national attention for North Carolina on sea level rise” (2013).

If you’re interested in a good summary of sea level rise policy in states, see this 2012 legislative report by Kristin Miller, et. al. (Connecticut General Assembly). It includes an analysis of sea level rise related policy in ten states (Louisiana, Florida, Maryland, Massachusetts, New Jersey, New York, North Carolina, Rhode Island, South Carolina and Virginia.)

Update: Check out Nickolay Lamm’s Sea Level Rise Images Depict What U.S. Cities Could Look Like In Future (PHOTOS) – click here. 

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.

The Love Lives of Horseshoe Crabs, Not Cannibals

Amidst the studies on Hurricane Sandy’s impacts on coastal communities—which affected the lives of people, most notably—some recent studies have examined the impacts on the lives of a strange ancient creature: horseshoe crabs. Distant relatives of scorpions and spiders, horseshoe crabs are not true crabs, or crustaceans. They’ve been around for over 1 billion years and lived alongside dinosaurs. See “The Life and Times of the Earliest Horseshoe Crabs,” (Rudkin, Royal Ontario Museum). Unlike a scorpion, crab or spider, horseshoe crabs don’t bite, sting or pinch. And unlike cannibalistic crustaceans, adult horseshoe crabs do not congregate (except to spawn seasonally), which is possibly a way to avoid large crabs attacking smaller horseshoe crabs—thus, avoiding cannibalistic behavior as a species. (Sekiguchi, Shuster, Jr., 1999) Their anatomy is interesting, as illustrated below.

Each spring, horseshoe crabs spawn along creek-mouth beaches and shoals. They like sandy beaches. Naturally, these coastal areas, rich in wetlands, peat bogs and saltwater marsh, were hit hard by Hurricane Sandy. What’s more, sea level rise has eroded certain coastal beaches where horseshoe crabs used to spawn, decreasing the habitat suitable for spawning. See Sea Level Rise and the Significance of Marginal Beaches for Horseshoe Crab Spawning (Botton and Loveland, 2011).

In the Delaware Bay, for example, the American Littoral Society, along with the Wetlands Institute, the New Jersey Department of Environment Protection and New Jersey Audubon, have assessed the impacts of Hurricane Sandy on horseshoe crab populations in the Bay. Watch this video of horseshoe crab spawning in Delaware. Read Hurricane Sandy Race To Restore Horseshoe Crab Spawning Grounds (March 2013). Videos depict horseshoe crabs spawning, swimming upside down and righting themselves.

In a joint report by the Wetlands Institute, NJ Audubon Society and NJ Division of Fish & Wildlife (“Damage from Superstorm Sandy to Horseshoe Crab Breeding and Shorebird Stopover Habitat on Delaware Bay,” December 2012), wetlands did well overall, despite some “wash over” during storm surges of Hurricane Sandy, according to Lenore Tedesco, Ph.D. Director of Research at the Wetlands Institute. Yet a major finding was a 70% decrease in suitable breeding habitat for horseshoe crabs. In addition, there was about the same amount of increase in unsuitable habitat for horseshoe crab spawning. Specifically, the scientists classified the types of habitat into five categories:

  1. Optimal: undisturbed sand beach;
  2. Suitable: sand beach with only small areas of peat and/or backed by development
  3. Less Suitable: exposed peat in lower/middle intertidal zone;
    sand present in upper intertidal;
  4. Avoided habitat:  exposed peat or active salt marsh fringing the shoreline;
    no sand present
  5. Disturbed due to beach fill, riprap or bulkheading.
    (Niles, Tedesco, Sellers, et. al. 2012)

In areas where the habitat is less suitable, with exposed peat, there is less sand for the horseshoe crabs to lay their eggs. The full report includes recommendations for habitat restoration. For more information about post-Sandy restoration recommendations, visit the Wetlands Institute’s website here.

Many years ago, I learned that horseshoe crabs (Limulus polyphemus) lay at the heart of some medical advances in immunology research. Apparently, horseshoe crab blood and immunology can serve scientists with a model to develop treatments for patients with HIV, AIDS or other immune deficiency disorders. Its “blue blood” contains Limulus Amebocyte Lysate, which allows medical researchers to detect bacterial toxins. In ecological projects, the spawning and genetic diversity of horseshoe crabs is the focus, or the relationship between horseshoe crabs and fisheries. For an overview of various research projects on horseshoe crabs happening in 18 states and two countries, see these project summaries. There’s some fascinating research underway.

The Wetland Institute has a number of publications on its website related to horseshoe crab research and conservation. There’s also an “Adopt a Horseshoe Crab” program and horseshoe crab census data available from 1999-2009. In May, the Institute holds festival activities, including teaching tank/aquarium talks on saltmarsh ecology, shorebirds and horseshoe crabs. For more information about the Horseshoe Crab Festival in May,click here.

More videos:

See horseshoe crab counting (Washington Post video, June 2012)
NATURE program on horseshoe crabs (PBS, 2008)
Horseshoe crab documentary (Nick Baker, Science Channel)

For more on horseshoe crab biology and ecology, see this National Park Service webpage and materials developed by the Mid-Atlantic Sea Grant and NOAA joint programs on horseshoe crab research. Finally, check outhttp://horseshoecrab.org/ which houses an online warehouse of information on the biology, conservation and research of horseshoe crabs.

Afflicted Bats Need Avengers; Bat Counters Needed

Lots of people are talking about “Batman.” Why did the “dark knight” choose bats as a symbol for his vigilantism?  In the comics, Bruce Wayne creates his ‘Batman’ identity when he conquered his childhood fear of bats. He created the illusion of having the speed, agility and nocturnal instincts of the only mammal able to sustain flight: the bat.

Although some people readily see the value of bats—including wetlandkeepers—other people are afraid of bats. Myths about bats, such as that bats carry rabies, are unfounded. Less than 1% of bats carry rabies. An individual is more likely to come across a skunk or domestic dog with rabies, than to encounter a bat with rabies. However, it is likely nowadays to find a bat infected with another disease. That is, if you can find a bat at all. Bats are sending up their own “bat-signal” of distress and need our help.

Currently bats in the U.S. are suffering the plight of white nose syndrome, a deadly fungus infection affecting a growing number of bat populations in North America. It started in New York in a bat colony in 2006. The fungus, Geomyces destructans, is considered an invasive species (Lanwig, Frick, et. al. Ecology Letters, 2012). Five years later, the disease has spread to 19 different states.  The death toll of North American bats succumbing to white nose syndrome was 5.5 million as of January 2012.

Myth: Bats will (not) entangle in your hair. Fact: Bats are natural pest control for crops. Myth: Bats suck blood. Fact: You’d have to leave the United States to find a vampire bat. The most common bats in the United States eat insects. Those of us in mosquito-stricken areas of the country, like Maine, are aware of bats’ ability to consume thousands of mosquitoes in a single night. Bats like to swoop through wetlands and riparian areas, and in turn, bat guano fertilizes vegetation. What most people don’t know is that “bat guano is big business” outside the U.S. as a source of fertilizer.  Also see: Effects of wetland network distribution on bat activity.

The most recent studies show that the more “social” the bats are, the tighter the cluster of bats in a colony, the more likely the disease is to spread. The grim reality is that the fungus has wiped out bat populations by the hundreds of thousands throughout the country. It’s in Delaware. It’s in Missouri. It’s in Kentucky, Ohio and Tennessee.  White nose syndrome has been confirmed in Wyoming and Maine, too. The U.S. Fish and Wildlife Service released a protocol for treatment and reduction of spreading the white nose syndrome in June 2012. For instance, if you handle a bat with white nose syndrome while wearing gloves, be sure to wash the gloves in hot water afterwards.

What’s strange is that not every bat infected with the fungus is dying. Sometimes a bat infected with white nose syndrome can live for a full year or longer after infection. In other cases, such as the big brown bat, scientists don’t know how the bats are avoiding the white nose syndrome; it might have to do with migrating south as opposed to huddling together in the infected caves, where the fungus is present. The endangered Indiana bat has not been hit as hard as biologists feared (their population is down about 70%).  One of the most common bats in the Northeast, the little brown bat, has taken a nosedive –its population plummeting by 90% due to white nose syndrome. SeeNortheastern Bat Update and Bats on the Brink.  There has been some hope in Vermont, New York and New Hampshire:  some of the little brown bat colonies are surviving and having pups, based on reports from state Fish and Game agencies. State agencies are calling for citizens to count bats and help promote awareness about them. In addition to research in the U.S., this year happens to be ‘Year of the Bat’ for international research and awareness about bats across the globe.

For the FWS’ blog on White Nose Syndrome, visit:http://whitenosebats.wordpress.com/
For information on Vermont’s Bat Program, click here.
For information on New Hampshire’s Bat Program, click here. 
For National Park Service (KY)’s Bat Program, visit:http://www.nps.gov/maca/whitenose.htm
Also see related blog post, White-nose syndrome confirmed in endangered gray bats

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

Dating Season for Toads

I am glad I don’t suffer bufonophobia, a fear of toads, because a gang of American toads (Bufo americanus) live under my deck. They come out at night and sit, fat as golfballs, one of them the size of a baseball, in the moonlight. Their posturing reminds me of the T-birds and the Pink Ladies in “Grease” at the drive-in.

Careful not to step on them when I stand in the yard, I let my dog enjoy a few minutes of midnight sounds, smells and shadows, with caution. The toads barely budge if she sniffs their bumpy bodies. She doesn’t like toads, luckily. I’m nervous about taking a step, worried I might squish one, anticipating the inevitable movement—but a toad’s test of wills (or staying power) beats mine every time.

Some toads, including the American toad, have paratoid glands that can secrete a white poison to would-be predators (if bitten or handled, for instance). The poison is toxic inside a mouth—or if after a human handles a toad, touches the eye or mouth.  It can cause nausea, inflamed mouth or throat, irregular heart beat and in very severe cases—death. They can be a danger to pets for this reason. When you think about it, batrachophobes, who fear any reptiles or amphibians, have probably had an incident that caused a symptom, or knew of someone who did. I never believed one could get “warts” from a toad, but perhaps this myth originated from the handling of toads causing undesirable symptoms. National Geographic busted that myth for kids, here.

Toads are nocturnal. During the day the amphibians hide under the deck. I’ve wondered what they do all day—eat insects, sleep, burrow underground, intimidate baby garter snakes? The child in me imagines Toad and Frog riding around in their small motorcar. The ecologist in me wants to set up candid cameras under the deck and film the toads’ daytime activities.  This is their breeding time (March-July), when they emerge from their burrows to eat at night and mate. It is more likely that the underside of my short deck is dull by day and hoppin’ at night. Along patches of my seep, nicknamed “Fern Gully,” I’ve observed toadlets, baby toads, crawling along the muddy wooded floor. They are small, about an inch long in body, not counting legs. What’s amazing to me is that toad eggs can hatch in a matter of days (3-13 days) and the toadlets grow to adulthood in about a month. In Pennsylvania, there is an organization looking for volunteers to help with a program called “Toad Detour,” that seeks to help toadlets cross roads and get to safe habitats. Their website has some great photos and a recording of toad sounds. More about their work with toads is posted on the Philly Herping Blog.

My poem, “Romancing the Toad,” was published in a summer issue of the international literary magazine, Off the Coast. 

The American toad’s large range extends as south as Georgia, as west as Wisconsin and as north as Canada. There are other toads of concern throughout the U.S. For example, the endangered Arroyo toad in California depends on adiminishing wetland habitat. The Sheepscot Wellspring Land Alliance for Spring Amphibians kicked off its programs in Maine earlier in May, teaching people about the 9 species of frogs and toads in the state.

In other blogs, spadefoot toads have received some attention lately. Volunteers in different areas gather to help toads and frogs cross busy roads during their breeding season. A headstart program in Massachusetts visited the Cape Cod National Seashore this month to learn about vernal pools and amphibian habitat, includingspadefoot toads. According to Mass Audubon, the spadefoot is neither true toad or frog—it’s a primitive amphibian. A segment of a Hands-On Wetland Creation Workshop for Professionals, led in part by Tom Biebighauser, with the U.S. Forest Service, addressed the topic of spadefoots at the Long Pasture Sanctuary on Cape Cod. ASWM’s Executive Director, Jeanne Christie, attended.