My Drive Across Canada: Part 2—Boreal Forest

The second leg of my drive west from Peterborough, took me past Thunder Bay, northwest from Lake Superior and into the heart of the boreal forest. Named after Boreas, the Greek god of the Northwind, the boreal forest is also called taiga (a Russian word from Yakut origin that means “untraversable forest”). Canada’s boreal forest is considered the largest intact forest on Earth, with around three million square kilometres still undisturbed by roads, cities and industrial development.

Canaada’s Boreal Forest

The boreal forest is the largest forest region in Ontario, covering two thirds of the province—some 50 million hectares—from the Great Lakes-St. Lawrence forest to the Hudson Bay Lowlands. 

I drove the Trans-Canada Highway (Hwy 17) through mixed coniferous forest, wetlands and marsh. The highway generally marks the boundary or transition zone between true Boreal Forest and the Great Lakes-St. Lawrence Forest, both dominated by coniferous trees.

Marshy river and spruce forest, north of Wawa, ON (photo by Nina Munteanu)

I stopped at English River overnight and the following morning woke to the echoing calls of two loons on the lake. I left at dawn with a peach sky behind me and a dark charcoal sky ahead of me. Soon the dark clouds unburdened themselves and the rain fell in a deluge as I continued west, barely making out the dense forest through flapping windshield wipers. The forest here was a mix of balsam fir, white and black spruce, white pine, aspen and white birch.

Spruce forest with birch and ground cover of moss and lichen, off Trans-Canada Highway, ON (photo by Nina Munteanu)

When the rain abated to a steady sprinkle, I ventured out to photograph the spruce-moss-lichen forest by the side of the road. I stood in the drizzle and set up my tripod and camera to take my shots, careful not to tread on the reindeer lichen. Reindeer lichen is highly susceptible to trampling. Branches break off easily and they take decades to recover. This foliose lichen is a key food source for reindeer and caribou during the winter; it also helps stabilize soil and recycles nutrients.

Spruce-moss-lichen forest off Trans-Canada Highway, ON (photo by Nina Munteanu)
Spruce-moss-lichen forest by Trans-Canada Highway, ON (photo by Nina Munteanu)

I drove into the tiny community of Vermillion Bay on Highway 17, looking forward to stopping in Quacker’s Diner for a hearty breakfast as advertised by a fetchy sign on the road. Alas, the place had closed long ago, according to the lady at the Moose Creek Trading Co., and hadn’t been replaced. And she couldn’t suggest anything else in the village. Disappointed, I felt I was truly in the middle of nowhere…

Sign for Nowhere, ON (photo by Nina Munteanu)

Then, a ways down the main road, I spotted the sign: “Nowhere Craft Chocolate & Coffee Roastery” and felt like I’d entered a dream-state where the north was run by hipsters.

Benny reaches Nowhere in Ontario, Vermillion Bay (photo by Nina Munteanu)

It was a husband and wife team who ran this wonderful craft bean-to-bar chocolate making and coffee roasting enterprise.

Filling my dark roast coffee order (photo by Nina Munteanu)

No sooner had I started to feel like I was back in trendy southern Ontario, when I met one of the locals, Simon, who worked in the bush and was patiently waiting for some dark roasts to take back to his buddies. We got to chatting and he shared some colourful stories about ‘the bush’ and folks who live in it, reminding me where I really was.

Coffee in hand, Simon stands next to his ATV with cooler, ready to return to ‘the bush’ with coffee (photo by Nina Munteanu)

When I mentioned the experience to a friend, she made the astute comment: “It is somehow satisfying to think of loggers and trappers and campers emerging out of the forests to go have a great cup of coffee and a hunk of chocolate. Why does that seem totally normal for Canada?”

Coffees from Nowhere
Chocolates from Nowhere

The Nowhere craft chocolate I bought—dark chocolate infused with ginger and Colombian coffee—was the best chocolate I’ve tasted this side of Switzerland. I bought some dark blends of Nowhere Coffee and continued my journey, happy despite no breakfast.

Black Spruce Forest

The black spruce (Picea mariana) dominates much of Canada’s boreal forests, frequently occurring in the Canadian Shield ecoregion where it forms extensive stands with groundcover of various mosses and reindeer lichen. Which of the two groundcover types depends on soil conditions and gaps in the forest from disturbance or fire.

Black spruce forest with moss and lichen ground cover, east of Dryden, ON (photo by Nina Munteanu)

The black spruce tree thrives in acidic peatlands, bogs and poorly drained mineral soils in wet, cold environments, but also grows in drier soils. It is particularly common on histosols (soils with peat and muck) on the Canadian Shield. Fires play a significant role in its regeneration as it replaces pioneer species such as white birch and tamarack after a fire, and grows with lichen and moss.

Marshland with black spruce, boreal forest north of Wawa, ON (photo by Nina Munteanu)

Mosses & Lichen Groundcover of Spruce-Dominated Forest

Both mosses and lichen (particularly reindeer lichen) help cool the forest by regulating evaporation and soil temperature; they can also fix nitrogen from the air, providing this key nutrient to an often nitrogen-limited ecosystem.

Spruce forest with feathermoss ground cover, ON (photo by Nina Munteanu)

This spruce-moss woodland is typified by fairly dense closed canopy of black spruce (Picea mariana), along with white spruce (Picea glauca), balsam fir (Abies balsamea), paper birch (Betula papyrifera) and trembling aspen (Populus tremuloides); this association creates a fairly shaded environment on the forest floor, inviting groundcover of various mosses such as feathermosses and Sphagnum that thrive in stable moist, shaded conditions.

Various mosses that typify the spruce-moss woodland in the boreal forest: A. Ostrich Plume Moss (photo by iNaturist); B. Red-Stemmed Feathermoss (photo by Ohio Moss and Lichen Association); C. Glittering Feathermoss; and D. Haircap moss with sundew (photographs by Nina Munteanu)

Common mosses in the spruce-dominated forest include Knight’s Plume Moss (Ptilium crista-castrensis), Red-Stemmed Feathermoss (Pleurozium schreberi), Glittering Feathermoss (Hylocomium splendens), and various species of Sphagnum. Knight’s Plume Moss and Sphagnum are key carbon cyclers in the poorly drained acidic boreal forest, contributing significantly to net primary productivity. They decompose slowly, leading to substantial organic matter accumulation.  Sphagnum in particular influences soil organic matter and carbon consumption during wildfires. Due to their ability to retain water, their acidity and resistance to decay, Sphagnum plays a crucial role in both the development and long-term persistence of peatlands where black spruce likes to live.

Various species of Sphagnum: A. Sphagnum squarrosum; B.Sphagnum papillosum; C. Sphagnum magellanicum; and D. Sphagnum papillosum (photos by Nina Munteanu)
Gray Reindeer Lichen (Cladonia rangiferina) colonizing granite outcrop in Catchacoma Forest, ON (photo by Nina Munteanu)

Spruce-lichen woodlands are characterized by an open canopy of black spruce trees, often with jack pine (Pinus banksiana) and white birch (Betula papyrifera) and a ground layer of mostly lichens, particularly fruticose species such as Cladonia rangiferina, C. mitis and C. stellaris.  This association is typically found on well-drained, often drier soils and may experience more extreme temperature fluctuations than spruce-moss associations. Through their release of acids that break down rock and organic matter, fruticose lichens contribute to soil formation.

Close up of a similar reindeer lichen species, Cladonia uncialis with Bristly Haircap Moss, on Catch Rock, ON (photo by Nina Munteanu)

A dense Cladonia mat also creates a microclimate that helps retain moisture. Lichen may also inhibit spruce regeneration, maintaining the open, park-like nature of lichen woodlands through the release of allelochemicals, such as usnic acid, that inhibit growth of plants and other lichen. Spruce-lichen woodlands may represent a stage in forest succession moving toward a closed-crown forest and may result from fire and insect disturbances that create openings in the forest canopy.

Spruce forest, showing reindeer lichen ground cover in foreground closest to the highway and moss ground cover upslope, ON (photo by Nina Munteanu)

This is what I observed where I’d stopped the car by the side of the road; closer to the disturbance of the open road, reindeer lichens—likely Cladonia rangiferina, C. mitis and C. stellaris—formed a thick continuous mat on the ground, which was fairly open with young spruce growing here and there. Further up the slope, where the canopy became more closed with mature trees, the mosses dominated the ground.

Boreal Wetlands & Kabenung Lake

Wetland north of Wawa, ON (photo by Nina Munteanu)

On my drive through the boreal forest north of Wawa, I encountered extensive wetlands—mostly marshes, bogs and fens, forming winding networks of water habitats. These water features are key to the environment’s water regulation, excellent carbon stores and provide habitat for many species. Boreal wetlands are seasonally or permanently waterlogged (up to 2 metres deep) with plant life adapted to wet conditions, including trees, shrubs, grasses, moss and lichen. Organic wetlands (peatlands or muskegs) such as bogs and fens accrue deep organic deposits. Mineral wetlands (marshes, swamps and open water) have shallow organic deposits; these open water systems have nutrient-rich soils.

Kabenung Lake, ON (photo by Nina Munteanu)

I stopped at Kabenung Lake, considered a prime fishing lake, supporting diverse populations that include Northern Pike, Whitefish, Bass, Walleye, Brook Trout, Lake Trout, and Perch. Judging by the map, I had only a small view of the large convoluted 16 km long lake from the highway. The angler’s bathymetric map suggests a maximum depth of fifteen metres near the lake’s centre.

Kabenung Lake, north of Wawa, ON (photo by Nina Munteanu)

Before my journey west took me out of Ontario (and the boreal forest) into Manitoba’s flat prairie, I continued on the Canadian Shield across rugged terrain dominated by conifer trees with ancient Archean rock outcrops of granite and gneiss revealed in rock cuts on the highway. I reached Kenora, a charming old town with character architecture and a vibrant downtown. The town is located in the Lake of the Woods area, near the transition to the Great Lakes-St. Lawrence Forest to the south and the Aspen Parkland to the west. I saw lots of spruce, fir and pine alongside birch, maple and poplar. Lake of the Woods is a huge lake about 4349 km2 with over 14,000 islands with a highly convoluted shoreline and serves as an active hub for fishing, recreation and sightseeing.

Lake of the Woods Brewing Company, Kenora, ON (photo by Nina Munteanu)

In Kenora, I made a short stop at the craft brewery Lake of the Woods Brewing Company, bought some Sneaky Peach Pale Ale to take with me, and continued west to the Manitoba border.

Nina with her Sneaky Peach Ale, Kenora, ON

On my way, I had to stop the car to let a red fox cross the road. It looked like it owned the road, just sashaying across in a confident trot and smiling at me…Yes, smiling!

Benny on a road in the boreal forest, east of Kenora, ON (photo by Nina Munteanu)

References:

Houle, Gilles and Louise Fillon. 2003. “The effects of lichens on white spruce seedling establishment and juvenile growth in a spruce-lichen woodland of subarctic Québec.” Ecoscience 10(1): 80-84.

Payette, Serge, Najat Bhiry, Ann Delwaide and Martin Simard. 2000. “Origin of the lichen woodland at its southern range limit in eastern Canada: the catastrophic impact of insect defoliators and fire on the spruce-moss forest.” Canadian J. of Forest Res. 20(2).

Rydin, Håkan, Urban Gunnarsson, and Sebastian Sunberg. 2006. “The Role of Sphagnum in Peatland Development and Persistence.” In: Boreal Peatland Ecology, Ecological Studies 188, R. K. Wieder and D. H. Vitt (eds) Springer-Verlag Berlin Heidelberg, pp 47-65.

Nina Munteanu is a Canadian ecologist / limnologist and novelist. She is co-editor of Europa SF and currently teaches writing courses at George Brown College and the University of Toronto. Visit  www.ninamunteanu.ca for the latest on her books. Nina’s bilingual “La natura dell’acqua / The Way of Water” was published by Mincione Edizioni in Rome. Her non-fiction book “Water Is…” by Pixl Press(Vancouver) was selected by Margaret Atwood in the New York Times ‘Year in Reading’ and was chosen as the 2017 Summer Read by Water Canada. Her novel “A Diary in the Age of Water” was released by Inanna Publications (Toronto) in June 2020.

The Ecology of Story: Revealing Hidden Characters of the Forest

 Story is place, and place is character—Nina Munteanu

EcologyOfStory coverI remember a wonderful conversation I had several years ago at a conference with another science fiction writer on weird and wonderful protagonists and antagonists. Derek knew me as an ecologist—in fact I’d been invited to do a lecture at that conference entitled “The Ecology of Story” (also the name of my writing guidebook on treating setting and place as a character). We discussed the role that ecology plays in creating setting that resonates with theme and how to provide characters enlivened with metaphor.

Derek was fascinated by saprotrophs and their qualities. Saprotrophs take their nutrition from dead and decaying matter such as decaying pieces of plants or animals by dissolving them and absorbing the energy through their body surface. They accomplish this by secreting digestive enzymes into the dead/decaying matter to absorb the soluble organic nutrients. The process—called lysotrophic nutrition—occurs through microscopic lysis of detritus. Examples of saprotrophs include mushrooms, slime mold, and bacteria.

Recipearium CostiGurguI recall Derek’s eagerness to create a story that involved characters who demonstrate saprotrophic traits or even were genuine saprotrophs (in science fiction you can do that—it’s not hard. Check out Costi Gurgu’s astonishing novel Recipearium for a thrilling example). I wonder if Derek fulfilled his imagination.

I think of what Derek said, as I walk in my favourite woodland. It is early spring and the river that had swollen with snow melt just a week before, now flows with more restraint. I can see the cobbles and clay of scoured banks under the water. Further on, part of the path along the river has collapsed from a major bank scour the previous week. The little river is rather big and capricious, I ponder; then I consider that the entire forest sways to similar vagaries of wind, season, precipitation and unforeseen events. Despite its steadfast appearance the forest flows—like the river—in a constant state of flux and change, cycling irrevocably through life and death.

Cedar trunk base

Cedar tree (photo by Nina Munteanu)

As I’m writing this, the entire world struggles with life and death in the deep throws of a viral pandemic. COVID-19 has sent many cities into severe lock down to prevent viral spread in a life and death conflict. I’ve left the city and I’m walking in a quiet forest in southern Ontario in early spring. The forest is also experiencing life and death. But here, this intricate dance has seamlessly partnered death and decay with the living being of the forest. Without the firm embrace of death and decay, life cannot dance. In fact, life would be impossible. What strikes me here in the forest is how the two dance so well.

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Cedar log, patterns in sapwood (photo by Nina Munteanu)

I walk slowly, eyes cast to the forest floor to the thick layer of dead leaves, and discover seeds and nuts—the promise of new life. I aim my gaze past trees and shrubs to the nearby snags and fallen logs. I’m looking for hidden gifts. One fallen cedar log reveals swirling impressionistic patterns of wood grain, dusted with moss and lichen. Nature’s death clothed in beauty.

The bark of a large pine tree that has fallen is riddled with tiny beetle holes drilled into its bark. Where the bark has sloughed off, a gallery of larval tracks in the sapwood create a map of meandering texture, form and colour.

Beetle bore holes pine log

White pine bark scales with tiny beetle bore holes, Little Rouge, ON (photo by Nina Munteanu)

larval tracks in pine wood

Beetle larval tracks in pine sapwood (photo by Nina Munteanu)

Nearby, another giant pine stands tall in the forest. Its roughly chiselled bark is dusted in lichens, moss and fungus. The broad thick ridges of the bark seem arranged like in a jigsaw puzzle with scales that resemble metal plates. They form a colourful layered mosaic of copper to gray and greenish-gray. At the base of the tree, I notice that some critter has burrowed a home in a notch between two of the pine’s feet. Then just around the corner, at the base of a cedar, I spot several half-eaten black walnuts strewn in a pile—no doubt brought and left there by some hungry and industrious squirrel who prefers to dine here.

The forest is littered with snags and fallen trees in different stages of breakdown, decomposition and decay. I spot several large cedar, pine, oak and maple snags with woodpecker holes. The snags may remain for many decades before finally falling to the ground.

Fallen Heroes, Mother Archetypes & Saprophyte Characters

WoodpeckerHole on cedar

Woodpecker hole in a snag (photo by Nina Munteanu)

The forest ecosystem supports a diverse community of organisms in various stages of life and death and decay. Trees lie at the heart of this ecosystem, supporting a complex and dynamic cycle of evolving life. Even in death, the trees continue to support thriving detrivore and saprophytic communities that, in turn, provide nutrients and soil for the next generation of living trees. It’s a partnership.

Decomposition and decay are the yin to the yang of growth, writes Trees for Life; and together they form two halves of the whole that is the closed-loop cycle of natural ecosystems.

Snags and rotting logs on the forest floor provide damp shelter and food for many plants and animals. Most are decomposers, including earthworms, fungi, and bacteria. As the wood decays, nutrients in the log break down and recycle in the forest ecosystem. Insects, mosses, lichens, and ferns recycle the nutrients and put them back into the soil for other forest plants to use. Dead wood is an important reservoir of organic matter in forests and a source of soil formation. Decaying and dead wood host diverse communities of bacteria and fungi.

TurkeyTail fungus on tree-LR

Turkey tail fungus, Little Rouge woodland (photo by Nina Munteanu)

Mother Archetypes

Wood tissues of tree stems include the outer bark, cork cambium, inner bark (phloem), vascular cambium, outer xylem (living sapwood), and the inner xylem (non-living heartwood). The outer bark provides a non-living barrier between the inner tree and harmful factors in the environment, such as fire, insects, and diseases. The cork cambium (phellogen) produces bark cells. The vascular cambium produces both the phloem cells (principal food-conducting tissue) and xylem cells of the sapwood (the main water storage and conducting tissue) and heartwood.

stages of tree life

Forest ecologists defined five broad stages in tree decay, shown by the condition of the bark and wood and presence of insects and other animals. The first two stages evolve rapidly; much more time elapses in the later stages, when the tree sags to the ground. These latter stages can take decades for the tree to break down completely and surrender all of itself back to the forest. A fallen tree nurtures, much like a “mother” archetype; it provides food, shelter, and protection to a vast community—from bears and small mammals to salamanders, invertebrates, fungus, moss and lichens. This is why fallen trees are called “nursing logs.”

uprooted stump carbon cushion fungus

Uprooted tree covered in fungi, lichen and moss, Little Rouge, ON (photo by Nina Munteanu)

 

Heralds, Tricksters and Enablers

rotting maple log2

Rotting maple log (photo by Nina Munteanu)

I stop to inspect another fallen tree lying on a bed of decaying maple, beech and oak leaves. When a fallen tree decomposes, unique new habitats are created within its body as the outer and inner bark, sapwood, and heartwood decompose at different rates, based in part on their characteristics for fine dining. For instance, the outer layers of the tree are rich in protein; inner layers are high in carbohydrates. This log—probably a sugar maple judging from what bark is left—has surrendered itself with the help of detrivores and saprophytes to decomposition and decay. The outer bark has mostly rotted and fallen away revealing an inner sapwood layer rich in varied colours, textures and incredible patterns—mostly from fungal infestations. In fact, this tree is a rich ecosystem for dozens of organisms. Wood-boring beetle larvae tunnel through the bark and wood, building their chambers and inoculating the tree with microbes. They open the tree to colonization by other microbes and small invertebrates. Slime molds, lichen, moss and fungi join in. The march of decay follows a succession of steps. Even fungi are followed by yet other fungi in the process as one form creates the right condition for another form.

rotting maple log

Rotting maple log, covered in carbon cushion fungus, Little Rouge, ON (photo by Nina Munteanu)

Most hardwoods take several decades to decompose and surrender all of themselves back to the forest. In western Canada in the westcoast old growth forest, trees like cedars can take over a hundred years to decay once they’re down. The maple log I’m studying in this Carolinian forest looks like it’s been lying on the ground for a while, certainly several years. The bark has fragmented and mostly fallen away, revealing layers of sapwood in differing stages of infestation and decay. Some sapwood is fragmented and cracked into blocks and in places looks like stacked bones.

Black lines as though drawn by a child’s paintbrush flow through much of the sapwood; these winding thick streaks of black known as “zone lines” are in fact clumps of dark mycelia, which cause “spalting,” the colouration of wood by fungus. According to mycologist Jens Petersen, these zone lines prevent “a hostile takeover by mycelia” from any interloping fungi. Most common trees that experience spalting include birch, maple, and beech. Two common fungi that cause spalting have colonized my maple log. They’re both carbon cushion fungi.

Spalting

Spalting through zone lines by carbon cushion fungus, Little Rouge, ON (photo by Nina Munteanu)

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Hypoxylon fungus (photo N. Munteanu)

Brittle cinder (Kretzschmaria deusta) resembles burnt wood at maturity. Deusta means “burned up” referring to the charred appearance of the fungus. Hypoxylon forms a “velvety” grey-greenish cushion or mat (stroma). As the Hypoxylon ages, it blackens and hardens and tiny, embedded fruitbodies (perithecia) show up like pimples over the surface of the crust.

Blue-green fungus on log

Green and Blue Stain fungus (photo N. Munteanu)

Much of the exposed outer wood layer looks as though it has been spray painted with a green to blue-black layer. The “paint” is caused by the green-stain fungus (Chlorociboria) and blue-stain fungus (Ceratocystis). The blue-green stain is a metabolite called xylindein. Chlorociboria and Ceratocystis are also spalter fungi, producing a pigment that changes the color of the wood where they grow. While zone lines that create spalting don’t damage wood, the fungus responsible most likely does.

Spalting is common because of the way fungi colonize, in waves of primary and secondary colonizers. Primary colonizers initially capture and control the resource, change the pH and structure of the wood, then must defend against the secondary colonizers now able to colonize the changed wood.

Intarsia using blue-green spalted wood

Details of 16th century German bureaus containing blue-green spalted wood by the elf-cup fungus Chlorociboria aeruginascens

Wood that is stained green, blue or blue-green by spalting fungi has been and continues to be valued for inlaid woodwork. In an article called “Exquisite Rot: Spalted Wood and the Lost Art of Intarsia” Daniel Elkind writes of how “the technique of intarsia–the fitting together of pieces of intricately cut wood to make often complex images–has produced some of the most awe-inspiring pieces of Renaissance craftsmanship.” The article explores “the history of this masterful art, and how an added dash of colour arose from the most unlikely source: lumber ridden with fungus.”

Shapeshifting Characters

moss hiding under leaves

Moss in forest litter (photo by Nina Munteanu)

I find moss everywhere in the forest, including beneath the forest floor. Moss is a ubiquitous character, adapting itself to different situations and scenarios. Like a shapeshifter, moss is at once coy, hiding beneath rotting leaf litter, stealthy and curious as it creeps up the feet of huge cedars, and exuberant as it unabashedly drapes itself over every possible surface such as logs, twigs and rocks, and then proceeds to procreate for all to see.

Moss is a non-vascular plant that helps create soil; moss also filters and retains water, stabilizes the ground and removes CO2 from the atmosphere. Science tells us that mosses are important regulators of soil hydroclimate and nutrient cycling in forests, particularly in boreal ecosystems, bolstering their resilience. Mosses help with nutrient cycling because they can fix nitrogen from the air, making it available to other plants.

Moss with spores water drops2

Green moss gametophyte with sporophytes growing out of it (photo by Nina Munteanu)

Mosses thrive in the wet winter and spring, providing brilliant green to an otherwise brown-gray environment. Even when covered in snow (or a bed of leaves), moss continues its growth cycle, usually in the leafy gametophyte stage. When the winter is moderate, like it is near Toronto, sporophyte structures can already appear on stalks that hold a capsule full of spores.  In the spring the capsules release spores that can each create a new moss individual. Moss is quietly, gloriously profligate.

Symbiotic Characters

Many twigs strewn on the leaf-covered forest floor are covered in grey-green lichen with leaf-like, lobes. On close inspection, the lichen thallus contains abundant cup-shaped fruiting bodies. I identify the lichen as Physchia stellaris, common and widespread in Ontario and typically pioneering on the bark of twigs—especially of poplars, and alders.

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Physchia stellaris lichen with fruiting bodies (apothecia), Little Rouge, ON (photo by Nina Munteanu)

Lichens are a cooperative character; two characters in one, really. Lichens are a complex symbiotic association of two or more fungi and algae (some also partner up with a yeast). The algae in lichens (called phycobiont or photobiont) photosynthesize and the fungus (mycobiont) provides protection for the photobiont. Both the algae and fungus absorb water, minerals, and pollutants from the air, through rain and dust. In sexual reproduction, the mycobiont produces fruiting bodies, often cup-shaped, called apothecia that release ascospores. The spores must find a compatible photobiont to create a lichen. They depend on each other for resources—from food to shelter and protection.

Forest as Character

Sunset 1 Niagara

Sunset in Niagara on the Lake (photo by Nina Munteanu)

In Far from the Madding Crowd, Thomas Hardy personified trees as interpreters between Nature and humanity: from the “sobbing breaths” of a fir plantation to the stillness of trees in a quiet fog, standing “in an attitude of intentness, as if they waited longingly for a wind to come and rock them.” Trees, meadows, winding brooks and country roads were far more than back-drop for Hardy’s world and his stories. Elements of the natural world were characters in their own right that impacted the other characters in a world dominated by nature.

Place ultimately portrays what lies at the heart of the story. Place as character serves as an archetype that story characters connect with and navigate in ways that depend on the theme of the story, particularly in allegories that rely strongly on metaphor. A story’s theme is essentially the “so what part” of the story. What is at stake for the character on their journey. Theme is the backbone—the heart—of the story, driving characters to journey through time and place toward some kind of fulfillment. There is no story without theme. And there is no theme without place.
—excerpted from The Ecology of Story: World as Character

 

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Nina Munteanu is a Canadian ecologist / limnologist and novelist. She is co-editor of Europa SF and currently teaches writing courses at George Brown College and the University of Toronto. Visit www.ninamunteanu.ca for the latest on her books. Nina’s bilingual “La natura dell’acqua / The Way of Water” was published by Mincione Edizioni in Rome. Her non-fiction book “Water Is…” by Pixl Press (Vancouver) was selected by Margaret Atwood in the New York Times ‘Year in Reading’ and was chosen as the 2017 Summer Read by Water Canada. Her novel “A Diary in the Age of Waterwill be released by Inanna Publications (Toronto) in June 2020.