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With temperatures rising, here comes ‘global weirding’

By John Waldman - posted Wednesday, 25 March 2009

They’re calling it “global weirding” - the way in which rising temperatures are causing species to change their ranges, the timing of their migrations, and the way they interact with other living things. And the implications of all this are only beginning to be understood.

The concept of “global weirding” is emerging as a notable complement to its cause, global warming. Coined by Hunter Lovins, a founder of the Rocky Mountain Institute, it describes the consequences of the rise in average global temperatures, which are expected to amplify the abnormal: hotter heat spells, longer and sharper droughts, more violent storms, and more intense flooding.

Given anticipated warming trajectories, many of these physical changes are statistically predictable and can be fairly accurately modelled. But as an ecologist, I fear it is the alterations to the living realm where “weirdness” will be a most apropos, if not downright tepid, label. This is certainly the case in my area of study - the aquatic realm - where global weirding is already well underway.


Forecasted biological changes due to warming often are as rudimentary as plots on maps where a species’ heat tolerances are superimposed on modelled temperature increases. This initial, or “first order,” assessment usually results in calculations of the species’ range shifting poleward - often accentuating actual movements already detected. Thus, if you live north of the equator you may learn that some beetle, bird, or vine is advancing from the south and may be seen in your backyard by 2018. New information, to be sure, but so what? What of its interactions with other organisms, including you? That is, how will it fit in the speedily evolving ecosystem and will it play a new role? And what of the effects of other species deserting locations they’ve long inhabited?

In New York’s Hudson River estuary, for example, rainbow smelt historically ran up its many tributaries, where they were enthusiastically netted for food as the first anadromous fish to appear each spring. But as a boreal species at the southern end of its range in a warming river, the Hudson’s rainbow smelt runs faded in the late 20th century, with the last individuals seen in 1998 - part of its general retreat northward from the waters of New York and southern New England.

During the same period, a southern fish - the gizzard shad - invaded the Hudson. Now in spring, this commercially worthless species gluts some of the same tributaries where smelt once ran. Existing in great numbers and biomass, the gizzard shad likely plays a significant but still undefined role in the Hudson, and it has since hopped from river to river as far north as Maine. The size of the ecological “hole” left by the rainbow smelt can only be speculated on.

The next, or “second order”, question of species interactions is far more complex. Ecology is a young field, with basic processes still under New York Department of Environmental Conservation investigation and the natural history information needed to minimally understand most creatures woefully inadequate. And yet, warming is forcing the planet to launch a giant ecological experiment in which organisms will increasingly interact with other organisms: Old dependencies will wither, while new contacts among them will emerge. Right now ecologists barely have the knowledge or tools to accurately predict the broader outcomes of changes to the simplest of interactions - between pairs of species.

But ecosystems are made up of myriad possible pairings, many exploitative in some way. Animals consume plants and also each other. The complexities embedded within a reasonably rich ecosystem are mind-boggling. Lake Okeechobee, Florida, has approximately 500 known species, but it is estimated that they engage in about 25,000 exploitative interactions. With warming, we can predict generally that there will be big winners, big losers, and draws among such species, but attempts to accurately predict these changes are far beyond our present capabilities.

A core biological issue with warming is that the very phenologies of plants and animals are changing. Phenology - a somewhat arcane word that, because of warming, is destined to become better known - means the relationship between physical conditions and the timing of ecological events. Lately, even relatively short-term monitoring is showing pronounced shifts towards earlier annual events, such as migrations associated with reproduction. The median nesting date for loggerhead turtles on Florida’s east coast, for example, has advanced 10 days in only 15 years; likewise, far up the Atlantic coast in Maine, the median date of capture of Atlantic salmon and alewife in two rivers has advanced more than a day a year in just 15 years. For both the turtles and the fishes, these advances in timing may create poorer matches to food sources - one more potential stress for species already in sharp decline.


A fundamental conflict underlying phenologies is that some life forms cue their annual life cycles to signals that haven’t changed - such as the northern hemisphere’s spring increase in sunlight - and others to temperature patterns, which are changing. The cumulative effects of changes in these linkages drive “third order” biotic changes - the broad community-wide shifts that are likely to affect the ways in which we live.

For example, in coastal waters of the northeastern US, the algae - or phytoplankton - that support the food chain bloom in late winter and early spring with the stimulus of increasing sunlight. Later, zooplankton that consume the algae ramp up reproduction after being stirred by rising water temperatures. The textbook model of this food chain contains enough of a time-lag between these episodes that the algae bloom reaches dense levels before being cropped by the zooplankton bloom, with excess, dying algae eventually spilling to the bottom as detritus that fertilises waters deeper than photosynthesis can occur. Without this supplement from above, much of the sea’s bottom waters would be biological deserts.

This process has long supported rich harvests of commercially important ground fishes. But now there is evidence from the northeastern US that the warmer waters allow the zooplankton bloom to occur earlier, shortening the lag following the algae bloom, which yields less detrital rain, at the cost of lessened production of bottom fishes. No one yet knows just how widespread this phenomenon is. But there is indication that top-water fishes have increased at the expense of bottom fishes in the North Atlantic, diminishing traditional fisheries.

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First published in Yale Environment 360 on March 19, 2009.

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About the Author

John Waldman, a professor of biology at Queens College, New York, works on the ecology and evolution of anadromous fishes, historical ecology, and urban waterways. Before joining Queens College, he worked for 20 years at the Hudson River Foundation for Science and Environmental Research. Waldman's recent books include Heartbeats in the Muck: A Dramatic Look at the History, Sea Life, and Environment of New York Harbor and The Dance of the Flying Gurnards: America's Coastal Curiosities and Beachside Wonders.

Creative Commons LicenseThis work is licensed under a Creative Commons License.

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