Although there are hundreds of examples of the interaction of climate change and biodiversity, there are three main poster children: impacts on polar wildlife such as seals, walruses, polar bears and penguins from the loss of sea ice; displacement and death by wildfires; and a warming ocean responsible for everything from the bleaching of coral reefs to the turbo charging of sea star wasting disease. The last falls under Chris Harley’s rubric of study, along with the related role of temperature close to the water’s surface.
Intertidal species already live close to their limits of thermal tolerance, meaning that even small temperature changes can have serious impacts. In a world only partially and periodically revealed, Harley studies not only thermal stress induced by rising temperatures, but how it affects competition, predation and disease.
At the Point Grey site, Harley is investigating why larger mussels fared worse during the heat dome than smaller, younger mussels packed tightly on different faces of the rocks. After an hour surveying the site where he set up an impromptu experiment of replicate larger-versus-small mussel plots, one thing is clear: the sudden deaths of billions of shoreline creatures surely affected tens of billions more in that web of life through loss of habitat. Based on observations made after previous heat waves — such as the disappearance of mussels from certain areas — some sites never re-establish similar faunas. The Inside Passage and coastal inlets such as Howe Sound, for example, are more sensitive to heat because they don’t have the direct moderating effect of the Pacific.
The heat dome also affected fieldwork conducted out of Harley’s lab in unexpected ways. Doctoral student Amelia Hesketh was looking at habitat-forming barnacles and their performance as builders in and out of sunlight. In the experiments she had set up, most unshaded barnacles died during the dome, while those under shade survived (inadvertently demonstrating the mortality effect). Sandra Emry, another doctoral student, was studying the effects of heat and salinity stress on seaweed using a propane heater, but air temperatures during the dome were higher than those she’d planned, throwing off her experiment.
As Harley focuses an infrared camera on his samples, he answers the question of whether wiping out this much of an ecosystem creates “vacant lots” more vulnerable to invasive species. “It’s actually worse,” he says. “The way the environment is changing may be favourable to things you don’t want to have dominate ecosystems, like toxic algal blooms and pathogens. The species dying at these temperatures are things like native mussels and low-shore kelp, and those doing well are Pacific oysters and orange-striped green anemones, both from Asia. The anemones definitely didn’t decrease, so they’re clearly not vulnerable.”
Shifting ranges and more heat-tolerant genotypes of native species likely won’t be enough to thwart the invaders, says Harley. “As it gets hotter, everything is sliding north, but not at the same speed,” he notes. “The Salish Sea is already a hot spot, and to find more heat-tolerant North American species you have to go to southern California or Mexico. So what’s going to happen here is it’s going to become more like Hong Kong and Japan. For instance, 15 years ago, the water rarely got warm enough for invasive Pacific oysters to spawn, but now it’s warm enough every year. When the dominant mussels get knocked back, it gives the oysters an advantage. The deeper clams are buried, the safer they are. But there are species differences, so invasive varnish clams that were buried 15 centimetres down survived, where more shallow-buried local heart cockles did not.”
In the end, intertidal ecosystems are like forest communities with a defined succession that starts with colonizer species. But no one knows what will happen now. “Phenology in intertidal organisms is governed by all the usual seasonal differences in temperature, salinity, light and food availability,” says Harley. “Like, are your larvae out there when there are things to eat?”
All that changes with events like the heat dome. “Ecosystems are complex, and when you make one change, you don’t know how it will affect all the other things keeping the system working.”
Visualizing the eviscerated shoreline as a metaphorical forest that has burnt to the ground offers an idea. Given that we’re in what writer Ed Struzik labels a “runaway fire age,” perhaps when it comes to water, heat is simply a new kind of fire.
In an article in the Tyee, Struzik explores what has supercharged the fire situation since 2003: a century of fire suppression that shifted forests from fire-resistant to fire-vulnerable; the draining of wetlands that can slow fires; the increasing popularity of rural properties among fire-foolish city-dwellers; lack of capacity for small communities to fire proof themselves; and, of course, climate change, with its skyrocketing temperatures and precipitation shifts driving the firestorms, fire tornados and lightning-producing fire clouds that make today’s wildfires larger, faster, deadlier and longer lasting.
Take the 2017 Plateau fire near Williams Lake, B.C.’s largest ever. I saw the aftermath up close on a rafting trip. As the Chilcotin River braided a valley near Alexis Creek, vegetated islands abounded, with squadrons of white pelicans, flocks of ducks, sandhill cranes and eagles that circled our flotilla expectantly, certain we were anglers who’d leave scraps in our wake. Then, with a suddenness that only river travel can bring, we swung into a canyon. The birds disappeared and the fire lines of 2017, visible for days on the horizon, descended in a monochrome of ash and charred trunks toppled into a disquieting jumble over ground rendered bare when the soil itself had burned off. The devastation was mind-boggling, more so when imagining the massive amounts of carbon that had vanished into the atmosphere in a geologic instant to add to our current climate woes. Then there was the impact on wildlife, and the loss from nature’s larder it represented to First Nations.
As an example of how drastically wildfires can shrink biodiversity, the 2019-20 Australian bushfires killed or displaced nearly three billion animals, a number that includes only those large enough to count and estimate — 2.46 billion reptiles, 143 million mammals, 180 million birds and 51 million frogs. Invertebrate losses were likely in the trillions. The fires that consumed the Brazilian and Bolivian Amazon in 2019 likewise killed an estimated 2.3 million animals, including already endangered species such as jaguars. There’s also a biohazard aspect: microbes and fungal spores can survive in wildfire smoke. According to the U.S. Centers for Disease Control and Prevention, as more wildfires plague California and Arizona, incidences of valley fever, a rare and potentially deadly fungal infection, rose sixfold from 1998 to 2018. Firefighters are especially vulnerable to the infection, which adds to the risk of inhaling smoke. What’s happening to animals that can’t put on a mask?
Given that northern latitudes are heating up faster than other parts of the planet, Canada is going to have to expect these kinds of unexpected events. And if this has echoes of the Rumsfeld Paradigm of known knowns, known unknowns and unknown unknowns, it shouldn’t surprise anyone. “When UBC climate professor Simon Donner was asked ‘Is this the new normal?’ he answered that things were now changing so fast he didn’t think there was ever going to be anything we could describe as normal again,” notes Harley. “That stuck with me.”
Not only was it a powerful indictment of the heat dome event, but it suggests that crafting biodiversity policy and management will become even more difficult given an increase in events that will be impossible to predict.