Showing posts with label climate change. Show all posts
Showing posts with label climate change. Show all posts

Thursday, December 19, 2013

More links for 2013: the 'new' conservation, the IPCC report in haiku, and more.

Conservation science has been at the receiving end of some harsh criticisms in the last couple of years, particularly from the current chief scientist of the Nature Conservancy, Peter Kareiva (e.g. 1).  They have suggested that conservation science needs to be redefined and refocused on human-centred benefits and values if it is to be successful. Some pushback in the form of TREE article from Dan Doak et al. suggests that reframing conservation in terms of its human benefits is not the best or only solution.

In a similar vein, another new paper in TREE asks what issues should the conservation community be addressing. A short-list of 15 issues suggests highly specific problems that should be addressed soon, including the exploitation of Antarctica, rapid geographic expansion of macroalgal cultivation for biofuels, and the loss of rhinos and elephants.

Even if the official IPCC report proves too long or dry for the average person to read before the end of the year, there is also a haiku version. The pretty watercolour illustrations don't make the report any more cheerful, unfortunately.

Finally, a new journal, "Elementa: Science of the Anthropocene" seems positioned to focus precisely on these kind of issues. According to their website: 

"Elementa is a new, open-access, scientific journal founded by BioOne, Dartmouth, Georgia Tech, the University of Colorado Boulder, the University of Michigan, and the University of Washington.
Elementa represents a comprehensive approach to the challenges presented by this era of accelerated human impact, embracing the concept that basic knowledge can foster sustainable solutions for society....Elementa publishes original research reporting on new knowledge of the Earth’s physical, chemical, and biological systems; interactions between human and natural systems; and steps that can be taken to mitigate and adapt to global change. "


It will be interesting to see how it develops.





Thursday, December 5, 2013

What can the future of ecology learn from the past?

Ecology has been under pressure to mature and progress as a discipline several times in its short life, always in response to looming environmental threats and the perception that ecological knowledge could be of great value. This happened notably in the 1960s, when the call for ecology to be better applicable occurred in relation to the publication of Silent Spring and fears about nuclear power and the Manhattan Project. Voices in academia, government, and the public called for ecology to become a “Big Science”, and focus on bigger scales (the ecosystem) and questions. And yet, “[Silent Spring] brought ecology as a word and concept to the public…A study committee, prodded by the publication of the book, reported to the ESA that their science was not ready to take on the responsibility being given to it.”

Arguably ecology has grown a lot since then: there have been advances in statistical approaches, spatial and temporal considerations, mechanistic understanding of multiple processes, in the number and type of systems and species studied, and the applications being considered. But it is once again facing a call (one that frankly has been ongoing for a number of years) to quickly progress as a science. The Anthropocene has proven an age of extinctions, human-mediated environmental changes, and threats to species and ecosystems from warming, habitat loss and fragmentation, extinctions, and invasions abound. Never has (applied) ecology appeared more relevant as a discipline to the general public and government. This is reflected in the increasing inclusion of buzzwords like “climate change”, “restoration”, “ecosystem services”, “biodiversity hotspot”, or “invasion” as keys to successful self-justification. Also similar to the 1960s is the feeling that ecology is not ready or able to meet the demand. Worse, that the time ecology has to respond is more limited than ever.

This first point--that ecology isn’t ready--is repeated in Georgina Mace’s (the outgoing president of the British Ecological Society) must-read editorial in Nature. The globe is in trouble, from climate change, disease, overpopulation, loss of habitat and biodiversity and Mace argues that ecology is incapable in its current form of responding to the need. She suggests that unless ecology evolves, it will fail as a discipline. Despite the growth of ecology that followed the 1960s, it is still a 'small' discipline: collaborations are mostly intra-disciplinary, data has been privately controlled, and the tendency remains to specialize on a particular system or organism of interest. However, this 'small' approach provides very little insight into the big problems of today - particularly understanding and predicting how the effects of global change on ecosystems and multispecies assemblages. To Mace, the solution, the undeniable necessity, is for ecology to get bigger. In particular, collaborations need to be broader and larger, with data sharing and availability (“big data”) the default. Ecological models and experiments/observations should be scaled up so that we can understand ecosystem effects and identify general trends across species or systems. In this new 'big' ecology, “[g]oals would be shaped by scientists, policy-makers and users of the resulting science, rather than by recent publishing trends”. Making research more interdisciplinary and including end-product users would allow the most important questions to receive the attention they deserve.

The difficulty with the looming environmental crises and the pressure on ecology to grow, is that the important decisions to be made have to be made rapidly and perhaps without complete information. Often scientific progress is afforded the time for slow progression and self-correction. After all, change is costly and risky, it requires reinvesting effort and funding, and may or may not pay off, and so science (including ecology) is often conservative. For example, a conservative mind would note that Mace’s suggestions are not without uncertainty and risk. Big data, for example, is acknowledged to have its strengths and its weaknesses, it may or may not be the cure-all it is touted as. Regardless of the amounts of data, good questions need to be asked and data, no matter how high quality, may not be appropriate for some questions. Context is often so important in ecology that attempts to combine data for meta-analysis may be questionable. Long running arguments within ecology reflect the fear that making ecological research more useful for applications and interdisciplinary questions may come at the expense of basic research and theory. It seems then that ecology is in an even worse scenario than Mace suggests, since not only must ecology change in order to respond to need, but it also must predict with incomplete information which future path will be most effective.

So ecological science is at an important junction with choices to make about future directions, limits on the information with which to make those choices, little time to make them, and much pressure to make them correctly. Perhaps we can take some comfort from the fact that ecology has been here before, though. There are some lessons we can draw from ecology’s last identity crisis, both the successes and failures. The last round resulted in ecology gaining legitimacy as a science and being integrated into policy and governance (the EPA, environmental assessments, etc). It appears, particularly in some countries, that ecology is more difficult to sell to policy and government today, but at the very least ecology has established a toehold it can take advantage of. Ecology also tried to focus on bigger scales in the 1960s--the concept of the 'ecosystem' resulted from that time--but the criticism was that the new ideas about ecosystems and evolutionary ecology weren't well integrated into ecological applications, and so their effect wasn't as broad as it could have been. Concepts like ecosystem services and function today integrate ecosystem science into applied outputs, and the cautionary tale is the value of balancing theoretical and applied development. It also seems that ecology must first consider what its duty as a science is to society (Mace’s assumption being that we have a great duty to be of value), since that is the key determinate of what path we decide to take. Then, we can hopefully consider what have we done right in recent years, what have we done wrong, and then decide where to go from here.
Page from "Silent Spring", Rachel Carson.

Tuesday, November 26, 2013

Can you teach an old bird new (migratory) tricks?


Jennifer A. Gill, José A. Alves, William J. Sutherland, Graham F. Appleton, Peter M. Potts and Tómas G. Gunnarsson. 2013. “Why is timing of bird migration advancing when individuals are not?” Proc. B. Vol. 281, no. 1774.

Phenological responses have been used as one of the major indicators of climate change. The timing of flowering and fruiting, the return of migrant birds and insects from winter habitats are easily and often measured, and records going back decades or centuries sometimes exist. Most importantly, shifts in phenological indicators are some of the strongest connections between rising temperatures and biological and ecological responses (for example). There is plenty of evidence, for example, that some migrant bird species are returning to their breeding grounds earlier than ever. These migratory birds may be responding (via migration timing) to warming temperatures in several ways: there may be plasticity or flexibility in individual timing of migration which allows them to respond to changing temperature cues; or species may also show adaptation via changes in the frequency of individuals with different migratory timings (microevolution). In cases where migratory species are responding to climate change, distinguishing the mechanisms allowing them to do so is surprisingly hard. Early arrival of migratory bird species is often explained as being due to individual plasticity or flexibility in “choosing” the date of migration, but the majority of studies of this phenomenon include little or no information about individual behaviour, only changes in the mean date of arrival for the entire population.


For this reason, Gill et al. looked at individual, rather than average population, arrival dates for Icelandic black-tailed godwits in south Iceland. Icelandic black-tailed godwits (“godwits” for the sake of brevity) have shown significant advances in the last 20 years in the timing of their spring arrival to the shores of Iceland, and these advances appear to relate to increasing temperatures. The population has also been banded such that 1-2% can be individually identified and tracked throughout their migratory range. Although only adults (of unknown age) were banded at the start of the experiment in 1999, recently chicks have also been banded and released and so a wide range of demographic classes are included with the banded birds.
From Gill et al. 2013.

When Gill et al. looked at date of arrival across 14 years for each individual, their results were surprisingly clear and cohesive. As previously reported, the population mean date of arrival in South Iceland had advanced as much as 2 weeks. But, this advance is not reflected in individual timing of arrivals over that same period – if a bird tends to arrive on a given day, they will continue to arrive on approximately that day every year, independent of temperature conditions. Instead, the population trend appears to be driven entirely by birds born in recent years – young individuals (recently hatched) tend to have arrival dates much earlier than older individuals. At least for the godwits, population wide trends in migration dates are actually driven by only a subset of the individuals.

From Gill et al. (2013)
Often it is assumed that migratory birds are responding to warming temperatures on an individual level: individuals respond to changing cues, resulting in shifts in arrival date. This study suggests otherwise, and finds that the important mechanism is not individual plasticity or microevolution but rather related to demographic shifts in arrival time. As to why younger birds arrive earlier, it is not clear, but may relate to the observation that nest building and hatching dates are also advancing. It may be that natal conditions are important – the authors observed a variety of possibly inter-related changes such that hatching dates are advancing and chick sizes are increasing, and the suggestion that mortality rates of later arriving individuals may also be higher. "Environmentally induced advances in arrival dates of recruits could operate through: (i) carry-over effects of changing natal conditions, (ii) changing patterns of mortality of individuals with differing arrival times, or (iii) arrival times being initially determined by conditions in the year of recruitment and individuals repeating those timings thereafter."

These results make some predictions about which populations of migratory birds might have the most ability to respond to warming climate - most likely those with shorter migratory distances, shorter times to reproduction and shorter-lifespans (hence decreasing the lag-time required for the population to catch up to temperature). It may also have relevance for other non-bird species that also rely on careful timing between phenology and temperature. Correspondingly, it suggests limitations - if individual behaviour is so inflexible and constrained, our hopes that some species may respond to climate change with behavioural changes seem far to simplistic.

Monday, November 11, 2013

Exploring the intersection of conservation, ecology and human well-being

I've seen a number of articles recently that explore in different way the intersection of environment and ecology, conservation and human societies. In particular, Frontiers in Ecology and Evolution (the free ESA journal you are gifted as a member) has dedicated an entire issue to the question of climate impacts on humans and ecosystems, and the papers cover important topics relating to changing climate and its effects on biodiversity, ecosystem integrity and human societies. Economic predictions suggest costs from fires, drought, and rising sea levels: whether protecting ecosystems will preserve their function and so mediate these costs to humans and other organisms is explored in depth. Of course, scholarly papers can be impersonal, but another article about the struggles of Inuit in the north to adapt (or not) to changing ecosystems provides a smaller, more human look at climate, development, and cultural change. Another study predicts that for some cultures, climate change (and the resulting difficulties growing food, maintaining livelihoods, obtaining water and human health risks) may be too much for them to withstand.

Finally, a long-form story by Paul Voosen in The Chronicle of Higher Education asks "Who is conservation for?". While not a novel question, through interviews with Gretchen Daily and Michael Soule, Voosen does a thorough job of illuminating conservation biology in the context of real-world limitations and realities, historical precedents, ongoing tensions between new and old approaches to conservation, and economic development. In the end it asks what motivates conservation: do we conserve purely for the sake of biodiversity alone, for economic and functional benefits, for aesthetic reasons, for charismatic and at-risk species? As Voosen subtly hints in the article, if leading conservation biologists can't agree on the answer, will it ever be possible to be effective?


Slightly unrelated, but there is a great short film online about the life of Alfred Russel Wallace, the less celebrated co-discoverer of natural selection.

Sunday, April 28, 2013

Wine-ing about climate change


If you like wine, particularly Old World wines, a recent paper by Lee Hannah et al (PNAS 2013), suggests that climate change is going to put a dent in your drinking habits. One way of communicating the ecosystem and economic effects of global warming has been to relate them to products or factors that affect the general population directly (an approach which has had mixed success). Wine (from Vitis vinifera grapes) is a great focal product - the success and quality of winemaking depends on terroir, which results from local temperatures and soil moisture. Changes in climate suitability for grapes reflects changes in suitability for many other agricultural and native species. Also, the motivations behind examining the effects of climate change on vineyards is more than economic – viticulture particularly thrives in Mediterranean-type ecosystems (France, Spain, Italy, California, Chile, South Africa, and Australia), which are areas with particularly high biodiversity and endemism. Vineyards use large amounts of fresh water and house low numbers of native species – so changes in their location and size may have contrasting effects on native biodiversity, local economies, and water supplies.

Given these relationships, the authors suggest that modeling regional changes in viticulture suitability provides insight into changes in ecosystem services and diversity. They examined 17 possible climate  models (GCMs) to look at how appropriate conditions for viticulture might shift by 2050. More than 50% of the models predicted that traditional wine producing regions (Bordeaux and Rhône valley regions in France and Tuscany in Italy) will decline greatly. However, regions farther north in Europe may become increasingly suitable. 
From Hannah et al. 2013. PNAS. The percentage of GCMs supporting a prediction reflects the degree of certainty behind it. Click for larger image.
New World vineyards receive a less dire forecast – some areas in Australia, Chile, California, and South Africa will remain suitable for viticulture in the future and new areas to the north are likely to become available. According to model predictions, New Zealand may one day produce many times more wine than it does currently. Such predicted increases in wine production in novel regions may be accompanied by viticulture’s increased ecological footprint. Some shifts take advantage of high elevations with cooler temperatures, leading to the development of areas that are currently relatively preserved. Water usage demands are likely to be problematic in the future: for example, vineyards in Chile’s Maipo Valley rely on runoff mountain basins that are vulnerable to warming conditions.
From Hannah et al. 2013. PNAS. (CA, California floristic province; CFR, Cape floristic region (South Africa); CHL, Chile; MedAus, Mediterranean-climate Australia; MedEur, Mediterranean-climate Europe; NEur, Northern Europe; NMAus, non–Mediterranean-climate Australia; NZL, New Zealand; WNAm, western North America).

Wine is a useful focal point for another reason - it exemplifies the complicated nature of most predictions related to climate change: positive outcomes (increased wine production in NZ) may be linked to negative changes (threatened water supply and native diversity in these new areas). Wine producers in a number of regions have recognized the possible impacts of vineyards, and groups such as the Biodiversity and Wine Initiative in the Cape Floristic Region of South Africa, and the Wine, Climate Change and Biodiversity Program in Chile exist to reconcile conflicting interests. There may be ways to mediate the effects of changing climate on viticulture, including developing tolerant varieties, changing methodologies, or the separation of varieties from their traditional regions. 

Making predictions about how ecosystems will change in the future is still difficult. However, the climate envelope model approach is actually well suited for situations like human agriculture, where dispersal limitation, competition, and non-equilibrium conditions are unlikely to be an issue. Cultivated crops are limited mostly by human/economic motivation. The results across most models strongly support the idea that Mediterranean climate growing regions will experience decreased viticultural suitability. It is likely more difficult on a fine scale to determine which regions will become more suitable in the future (i.e. probably don’t invest in land in New Zealand, assuming you can start a vineyard there in 50 years) but the strong agreement between models suggests that you should enjoy some French or Italian wine sooner rather than later.



Tuesday, April 2, 2013

Carbon sequestration in boreal forests: below-ground interactions matter


One of the most important developments in plant ecology over the last 20 or so years is the inclusion of belowground interactions with fungi into traditional studies of plant diversity, productivity, and ecosystem functions. Results like those from van der Heijden (1998)--which showed experimentally that the assumed link between ecosystem function and plant diversity was actually driven by arbuscular mycorrhizal fungal diversity (through their effects on plant communities)—must alter how we see plant community dynamics. Not only does this reinforce the importance of complexity in ecology, but more specifically it suggests that if fungi are a necessary component of plant community identity and function, they must be explicitly considered in management and conservation plans.

For example, an important current issue is the question of which ecosystems will be carbon sinks as part of a focus on atmospheric CO2 levels. Understanding the mechanisms by which carbon is stored is therefore an important topic. Boreal forests sequester net amounts of carbon in soil and it is generally assumed that this is as a result of plant litter and organic matter accumulating in soil. Clemmensen et al. (2013) examined soil chronosequences for forested islands in Sweden to test whether this hypothesis held. These islands differed in the frequency of fire occurrences, between large and frequently burnt islands and smaller, infrequently burnt islands.

The authors identified the age since fixation of C found in the chronosequences and used models of C source to look at the relative contribution of the two possible processes: either fixation of C through aboveground plant litter or below-ground inputs through root-associated fungi. Carbon input tended to be higher on the small islands that were burnt less often, and this was associated entirely with root-derived input. Further, DNA barcoding showed that on these small islands, there were mycorrhizal fungi associated with the soil depths where the root-derived inputs were occurring. On islands which burned more frequently, and had lower carbon input, fungi were absent at these depths (figure below). This difference in fungal profile was related to the fact that infrequently burnt islands had older mycelium with low turnover, hence greater carbon sequestration.
From Clemmensen et al (2013). A) Fungal functional groups associated with soil depths on large, frequently burnt islands (panel 1) and small, infrequently burnt islands (panel 2).

The authors convincingly show that, at least in some ecosystems, the view that decomposition of litter primarily drives humus accumulation (and the accompanying carbon sequestration) must be tempered with the knowledge that organic layers also accumulate from below by roots and root-associated fungi. This suggests that there is a need to consider fungal communities as well as plant communities for when managing forests and making inventories of global carbon stores. And probably a need to consider fungi much more often in general.

Monday, March 18, 2013

Evolution on an ecological scale


Andrew Gonzalez, Ophélie Ronce, Regis Ferriere, and Michael E. Hochberg. 2013. Evolutionary rescue: an emerging focus at the intersection between ecology and evolution. Philos Trans R Soc Lond B Biol Sci. 368 (1610).doi: 10.1098/rstb.2012.0404 (Intro to special issue).

David A. Vasseur, Priyanga Amarasekare, Volker H. W. Rudolf, Jonathan M. Levine. 2011. Eco-Evolutionary Dynamics Enable Coexistence via Neighbor-Dependent Selection. The American Naturalist, Vol. 178, No. 5, pp.E96-E109.

Ecology and evolution are often treated as connected but ultimately discrete areas of study. Ecological processes are usually the main source of explanation for ecological patterns and  ecologists may ignore evolutionary processes under the assumption that these are most important over longer time scales than are of interest (e.g. speciation). However, there is also an increasing recognition that rapid evolutionary dynamics can contribute to ecological observations. In a time where rapid changes to climate and habitat are the greatest threats to most species, the suggestion that rapid evolution might play a role in extinction prevention and diversity maintenance is an important one.

Increasingly researchers are exploring this concept. The concept of evolutionary rescue (ER), has been particularly championed by Andy Gonzalez and Graham Bell of McGill University. ER results when evolution occurs fast enough to arrest population declines and allow populations to avoid extinction in the face of changing conditions. Changing conditions resulting in maladapted populations should result in population declines followed by extinction. However, if selection for resistant types (which are present in the population, or result from mutations) occurs, population declines can be countered. The result is a characteristic u-shape curve, showing the initial geometric decline, followed by a geometric increase – escape from extinction is then a balance between rates of evolution and success of resistant types compared to rates of population decline.
From Bell & Gonzalez 2009.
The question of whether evolution may have relevance to population declines is not precisely new, but it is especially relevant given we are in a period of habitat changes and extinction. A special issue of Proc B is focused only ER, on the question of its importance, prevalence, and predictability. Many of the articles extend theory, exploring assumptions about the type of environmental change, type and extent of the threat, presence of dispersal, spatial gradients, etc. A few articles attempt the more difficult task of testing for ER in natural systems and assessing its likely prevalence and value to conservation activities. It is an interesting journal issue and a great example of the importance of context in determining when an idea takes off. The theoretical background for evolutionary rescue has existed for many years, but it took the context of climate change (and perhaps the collaboration of an ecologist and evolutionary biologist?) for it to gain ground as an area of ecological research.

Another interesting paper, this one linking evolutionary dynamics with community coexistence, is from Vasseur et al. (2011). In this case, the authors suggest an evolutionary mechanism that could augment coexistence when ecological conditions allow for niche partitioning and that could allow coexistence when ecological conditions lead to competitive exclusion. If species exhibit tradeoffs between traits that are optimal for intraspecific interactions and traits that are optimal for interspecific interactions, evo-ecological dynamics can produce coexistence. Such tradeoff means that a species will be a superior interspecific competitor when rare and a poor interspecific competitor when common. Such a tradeoff creates neatly alternately selective pressures depending on whether a species is common (fitness declines) or rare (fitness increases). This is presented as a theoretical model, but it seems like in a tractable system one could easily test for changes in ecological and evolutionary pressures as predicted by the model.

No one would argue with the conclusion that a closer relationship between ecology and evolutionary biology would be beneficial for both. But in practice this seems to be the exception rather than the rule. "Evolutionary ecology" as it exists is fairly restricted, and if complaints about seminar topics is to provide a hint, most ecologists feel disconnected from evolutionary topics and vice versa. If evolutionary dynamics are relevant on an ecological scale, it seems that we should at least attempt to understand their prevalence and importance in natural systems.


Friday, September 23, 2011

NSF funds Project Baseline

NSF approved 1.2 million dollars for a unique and visionary idea: collect 12 million seeds and store them in seed banks for years to come. And while storing seeds for the future doesn't sounds so different from what other groups have already done, where Project Baseline differs is that this seed bank is not only a conservation measure--preserving natural genetic variation from plant populations for the future--but also an opportunity to track the effects of changing climate on the direction and rate of evolution in these species.

This idea was first explored in "The Resurrection Initiative: Storing Ancestral Genotypes to Capture Evolution in Action" (Franks et al 2007). By collecting and storing seeds from both within and across populations throughout the range of a species, ancestral and descendent populations can be compared in the not too distant future. The role of adaptive evolution and range shifts can be explored through this lens. Project Baseline is a great example of how much we can learn from long-term, collaborative experiments and projects (other examples include NutNet , NCEAS), and how valuable funding such projects should be considered.

Tuesday, January 25, 2011

Trend in ecology, 2010

Sciences are always in a state of ebb and flow (sorry), and topics of study fall in or out of fashion in response to paradigms shifts, methodological advances, and to support necessary ecological applications.
For the sake of curiosity, I've compiled the top keywords from ecology publications in 2010. Obviously there are many covariates, but it should come as no surprise that the top words were "biodiversity" (667 times), "climate change" (293), and "conservation" (274); other popular keywords were "evolution" (277), "population (ecology)" (273), and the rather vague "patterns" (196).

(click image for larger view)

Thursday, June 11, 2009

The sushi of tomorrow… Jellyfish rolls?

With the world’s fisheries teetering on the edge of collapse, familiar items at your local sushi bar might disappear in the near future. One candidate for replacing the Hamachi, Ikura, Maguru, Tai, and Toro on the menu is the jellyfish, which seems to be doing well – too well, actually – in today’s environment.

In recent years, jellyfish outbreaks have become more frequent and more severe. These outbreaks can have lasting ecological and economic consequences. They can wreak havoc on the tourist industry by closing beaches and harming swimmers, cause power outages by blocking cooling intakes at coastal power plants, reduce commercial fish abundance via competition and predation, spread fish parasites, burst fishing nets, and contaminate catches.

A review by Anthony Richardson and his collaborators suggests that human activities such as overfishing, eutrophication, climate change, translocation, and habitat modification have dramatically increased jellyfish numbers. Their research, which was published this week in Trends in Ecology and Evolution, highlights that the structure of pelagic ecosystems can abruptly transition from one that is dominated by fish to one that is dominated by jellyfish.

Richardson and his collaborators present a potential mechanism to explain how local jellyfish aggregations can spread, displace fish, and form an alternative stable state to fish-dominated ecosystems. Jellyfish are like the opportunistic weed of the sea, giving them an edge in environments stressed by climate change, eutrophication, and overfishing. In these disturbed environments, the abundance of jellyfish relative to filter-feeding fish increases until a tipping point is reached. Under normal conditions, filter-feeding fish keep jellyfish populations in check via competition for planktonic food and (perhaps) predation on an early life-stage of the jellyfish. At the tipping point, jellyfish numbers are such that they begin to overwhelm any control of their vulnerable life-cycle stages by fish predators. At the same time, jellyfish progressively eliminate competitors and predators via their predation on fish eggs and larvae. As jellyfish abundance increases, sexual reproduction becomes more efficient, allowing them to infest new habitats where fish might have formally controlled jellyfish numbers.

Richardson and his collaborators suggest that one way to hit the brakes on what they call the “the never-ending jellyfish joyride” is to harvest more jellyfish for human consumption. Jellyfish have been eaten for more than 1000 years in China, where they are often added to salads. In Japan they are served as sushi and in Thailand they are turned into a crunchy noodle concoction. Although the taste and texture of jellyfish might not be appealing to some westerners, I for one have yet to meet a sushi that I didn’t like. Of course, jellyfish harvesting is unlikely to return systems to their fish-dominated state if the stresses that caused the ecosystem shift remain.

Richardson, A. J., A. Bakun, G. C. Hays, and M. J. Gibbons. 2009. The jellyfish joyride: Causes, consequences and management responses to a more gelatinous future. Trends in Ecology and Evolution, 24 (6), 312-322 DOI: 10.1016/j.tree.2009.01.010

Wednesday, May 20, 2009

Fire and the changing world

ResearchBlogging.orgThis is probably the most appropriate blog I have ever written. My family and I were evacuated two weeks ago because of the Jesusita fire in Santa Barbara, and several homes in our neighborhood were lost. Here in Santa Barbara we have experienced multiple years of extremely large fires, with this last one occurring much earlier than previous fires.

Wildfires have been a part of the Earth’s biota likely since organisms first died and dried on land. Ecosystems have been shaped by fire, numerous organisms have evolved strategies to cope with fire and human cultural development has close tied to fire. In a recent review paper in Science by David Bowman, Jennifer Balch and colleagues, they asked the question: how have fires changed and what does the future look like? Human activities are changing fire patterns and climate change may be entering a feedback with fire. Global warming has been linked to increases in extreme fire weather, making large, destructive fires more probable. However, these large fires feedback into this loop because they release compounds that have strong greenhouse effects. Further, smoke plumes inhibit cloud formation, reinforcing the dry conditions that lead to the fires in the first place.

They argue that fire needs to be incorporating into models of climate change and especially those that link ecosystem properties climate change. Fire may change the distribution of specific habitat types beyond that predicting by responses to climate change alone.

Bowman, D., Balch, J., Artaxo, P., Bond, W., Carlson, J., Cochrane, M., D'Antonio, C., DeFries, R., Doyle, J., Harrison, S., Johnston, F., Keeley, J., Krawchuk, M., Kull, C., Marston, J., Moritz, M., Prentice, I., Roos, C., Scott, A., Swetnam, T., van der Werf, G., & Pyne, S. (2009). Fire in the Earth System Science, 324 (5926), 481-484 DOI: 10.1126/science.1163886

Tuesday, May 12, 2009

Hurricanes might contribute to global warming

In a large-scale study published this week in Proceedings of the National Academy of Sciences, Hongcheng Zeng and colleagues show that hurricane damage can diminish a forest’s ability to absorb carbon dioxide from the atmosphere. Their results suggest that an increase in hurricane frequency due to global warming may further amplify global warming.

The annual amount of carbon dioxide a forest absorbs from the atmosphere is determined by the ratio of tree growth to tree mortality each year. When hurricanes cause extensive tree mortality, not only are there fewer trees in the forest to absorb greenhouse gases, but these tree die-offs also emit carbon dioxide, thus potentially warming the climate.

Using field measurements, satellite image analyses, and empirical models to evaluate forest and carbon cycle impacts of hurricanes, the researchers established that an average of 97 million trees have been affected each year for the past 150 years over the continental United States, resulting in a 53-million ton annual biomass loss and an average carbon release of 25 million tons per year. Over the period of 1980–1990, released CO2 potentially offset carbon absorption by forest trees by 9–18% over the entire United States. Impacts on forests were primarily located in Gulf Coast areas such as southern Texas, Louisiana, and Florida, but significant impacts also occurred in eastern North Carolina.

These results have important implications for evaluating positive feedback loops between global warming and environmental change.


Zenga, H., J. Q. Chambers, R. I. Negrón-Juárez, G. C. Hurtt, D. B. Baker, and M. D. Powell. (2009). Impacts of tropical cyclones on U.S. forest tree mortality and carbon flux from 1851 to 2000. PNAS, 106 (19), 7888-7892. DOI:10.1073/pnas.0808914106

Sunday, April 5, 2009

Climate change increases West Nile Virus outbreaks in the U.S.

According to a study recently published in Environmental Health Perspectives, climate change has increased the prevalence of West Nile Virus infections in the United States. In one of the largest surveys of West Nile Virus cases to date, the authors find a correlation between increasing temperature and rainfall and outbreaks of the mosquito-borne disease between 2001 and 2005. Because warming weather patterns and increasing rainfall are both projected to accelerate with global warming, the authors predict that climate change will exacerbate West Nile Virus outbreaks in the future.

In the study, Dr. Jonathan Soverow and his collaborators matched more than 16,000 confirmed West Nile cases in 17 states to local meteorological data.

Warmer temperatures had the greatest effect on outbreaks. By extending the length of the mosquito breeding season and decreasing the amount of time it takes mosquitoes to reach their adult, biting stage, warmer weather means more biting mosquitoes longer. Moreover, increasing temperature speeds multiplication of the virus within insects, so mosquitoes in warmer climates have a greater viral load, making them more likely to infect humans.

Increased precipitation was also correlated with higher rates of West Nile Virus infection. A single, heavy rainstorm resulting in two or more inches of rain increased infection rates by 33%, while smaller storms had less of an effect on infection rates. Heavier rainfall events can increase disease prevalence by creating pools of water in which mosquitoes can breed and by increasing humidity, which stimulates mosquitoes to bite and breed. Total weekly rainfall had a smaller but significant effect on West Nile Virus infections, with an increase of 0.75 inch of rain/week increasing the number of infections by about 5%.

Warmer, wetter weather patterns might expand the niches of the mosquito species that carry West Nile Virus. In California, for instance, several mosquito species carrying the West Nile Virus have extended their ranges into higher elevations and coastal areas as temperatures have warmed. Changing weather patterns might also affect certain species of birds that are reservoirs for West Nile Virus. For example, droughts can push bird populations into urban areas, making West Nile Virus outbreaks in human populations more likely.

Soverow, J.E., G.A. Wellenius, D.N. Fisman, and M.A. Mittleman. 2009. Infectious disease in a warming world: How weather influenced West Nile Virus in the United States (2001-2005). Environmental Health Perspectives. Online 16 March 2009 DOI: 10.1289/ehp.0800487

Friday, March 6, 2009

Salamaders and climate change -impending extinctions?

ResearchBlogging.orgBy the now the evidence of a global frog decline, perhaps even an extinction crisis, has been well documented. But what about salamanders? They are normally less abundant and less-studied compared to frogs, but is there evidence of the same general pattern of declining population sizes? According to Sean Rovito and colleagues, the answer is unfortunately yes. They repeated a plethodontid (lungless) salamander survey done in the 1970’s in Central America and found that many species have declined. In fact they failed to find a couple of previously very abundant species. They also found that species declines were phylogenetically non-random and so these declines may result in the loss of whole clades of species, meaning that the evolutionary history of these salamanders is at risk.

The authors attempted to determine the cause of these declines and found that neither habitat loss or the chytridiomycosis fungal disease implicated in other declines explained these salamander declines. The authors hypothesize that these declines are a direct result of climate change –namely changing temperature and humidity. If so, we may be witnessing some of the first extinctions that are directly caused by climate change.

S. M. Rovito, G. Parra-Olea, C. R. Vasquez-Almazan, T. J. Papenfuss, D. B. Wake (2009). Dramatic declines in neotropical salamander populations are an important part of the global amphibian crisis Proceedings of the National Academy of Sciences, 106 (9), 3231-3236 DOI: 10.1073/pnas.0813051106

Post script:
We had a comment questioning the use of climate change as an explanation and here is my response.

Science works by finding parsimonious explanations, until through experimentation or observation another, better explanation emerges. The previous explanations of habitat loss or fungal infections were not supported. These habitats, known as cloud forests, are very humid. The lungless salamanders have no lungs and instead breath through their skin, which must be kept moist. These forest are becoming drier, hence the probable connection. Here's a quote from the paper:

"Pounds et al. (25) used modeling to show that largescale warming led to a greater decrease in relative humidity at Monteverde compared to that caused by deforestation. Species of cloud forest salamanders that can still be found rely at least
in part on bromeliads. Bromeliads depend on cloud water deposition and are predicted to be articularly vulnerable to climate change (26, 27)."

Doesn't sound like "magic" to me, rather a robust hypothesized mechanism worthy of more testing. Given that species are going extinct, it is important to suggest likely mechanisms, providing an impetus for more research.

For those that think that scientists use climate change as boogey man to scare up more research funding (i.e., Crichton), please read the science. You'll discover honest, hardworking folks that are trying to understand this changing world and whose research can only benefit you , me and the salamanders.