Jens-Christian Svenning | |
---|---|
Born | July 9, 1970 |
Nationality | Danish |
Occupation(s) | Ecologist and academic |
Awards | Ebbe Nielsen Prize, Global Biodiversity Information Facility (2011) EliteForsk Prize, Danish Ministry of Higher Education and Science (2014) Queen Margrethe II's Science Award, Royal Danish Academy of Sciences and Letters (2016) Distinguished Fellow, Chinese Academy of Sciences (2017) Annual Award in Science and Technology, Villum Foundation (2021) Ernst Haeckel Prize, European Ecological Federation (2022) Carlsberg Foundation Research Prize (2023) |
Academic background | |
Education | MSc., Biology PhD., Ecology |
Alma mater | Aarhus University Indiana University |
Thesis | Population and community ecology of Neotropical rain forest palms (Arecaceae) (1999) |
Academic work | |
Discipline | Macroecology Biogeography Global change Restoration and rewilding Human ecology |
Institutions | Aarhus University Smithsonian Tropical Research Institute |
Jens-Christian Svenning is a Danish ecologist,biogeographer and academic. He is a Professor at the Department of Biology at Aarhus University,Denmark where he also serves as the Director of DNRF Center for Ecological Dynamics in a Novel Biosphere (ECONOVO),established in 2023. [1]
Svenning is known for his research in macroecology,biogeography,biodiversity,the effects of climate change on biomes,rewilding,and human-environment interactions across historical and future contexts with a specific focus on concepts like disequilibrium dynamics and the impacts of top-down trophic processes. In 1995,he collected a specimen of a new species of pepper plant which was named after him as Piper svenningii. [2] He is the recipient of the 2011 Global Biodiversity Information Facility Ebbe Nielsen Prize, [3] the EliteForsk Prize from the Danish Ministry of Higher Education and Science in 2014, [4] the 2016 Royal Danish Academy of Sciences and Letters' Queen Margrethe II's Science Award, [5] Chinese Academy of Sciences' Distinguished Fellow Award in 2017,the 2021 Villum Kann Rasmussen Annual Award in Science and Technology of DKK 5 million, [6] the European Ecological Federation Ernst Haeckel Prize in 2022, [7] and the 2023 Carlsberg Foundation Research Prize. [8]
Svenning was elected as Fellow of the Royal Danish Academy of Sciences and Letters in 2010 and the Danish Academy of Natural Sciences in 2011. [9]
Svenning obtained a MSc in Biology in 1997 from Aarhus University. Subsequently,he received a PhD in Ecology from Aarhus University in 1999. [10]
Svenning began his academic career in 1999 as an Assistant Professor at the Department of Biological Sciences at Aarhus University,followed by a Postdoctoral position at the Smithsonian Tropical Research Institution during 2000-2002. In 2002,he became Assistant Professor at Aarhus University,later appointed Associate Professor in 2005,Professor (MSO) in 2009,and has been serving as Professor at Aarhus University since 2013. [1]
Svenning served as the Director of Center for Biodiversity Dynamics in a Changing World (BIOCHANGE) from 2017 to 2023. [11] In 2023,he was appointed as the Director of DNRF Center for Ecological Dynamics in a Novel Biosphere (ECONOVO). [12]
Svenning worked as Subject Editor of Ecography from 2005 to 2010 and Deputy Editor-in-Chief at the same journal since 2010, [13] and was also Associate Editor of the Journal of Biogeography from 2007 to 2019. He has served as Chair of the Maasai Mara Science and Development Initiative Scientific Board during 2015 –2018 and since then as Chair of the board. He has been serving as the Subject Editor for the Nordic Journal of Botany since 2007. [14] He has also been on the 15. Juni Fonden Board since 2018, [15] and Rewilding Europe Supervisory Board since 2020. [16] In addition,he was appointed to the Danish Biodiversity Council to provide expert advice to the Danish government and parliament in the Ministry of Environment of Denmark from 2020 to 2024. [17]
Svenning has contributed to the field of ecology by studying macroecology,biogeography,landscape ecology,community ecology,paleoecology,conservation and rewilding,human ecology,ecoinformatics,remote sensing,and global change biology including climate change and alien species invasions. [2] He has utilized and developed Big Data approaches based on large databases to handle and analyze advanced data in his research alongside field-based research. [18]
Svenning has studied basic biodiversity science and ecology throughout his career. As part of an international collaboration,he showed that processes influencing the latitudinal gradient in species richness are complex,with trait diversity in tree assemblages showing patterns consistent with environmental filtering theory at the alpha and beta scales,but no consistent support for any single theory at the gamma scale. [19] He also determined that microhabitat specialization,particularly related to topography,is a key factor in maintaining the diversity of palm species in YasuníNational Park. [20]
Svenning's work in biogeography has involved using a variety of methods to understand how different factors have influenced the distribution of species and ecosystems over time. Along with his collaborators,he found that plant range sizes are codetermined by habitat area and long and short-term climate stability. [21] He also participated in a study suggesting that past climate changes are linked to reduced spatial turnover and increased nestedness in angiosperm tree diversity worldwide,potentially foreshadowing homogenization and decreased diversity under future human-driven climate change. [22]
Svenning has examined the impacts of current and future climate change on biodiversity,ecosystems and people in many studies. In a study,he and his team revealed that global warming is leading to significant shifts in the distribution of tropical plant species,with evidence of upward movements of vegetation zones and individual plant taxa up to 500 meters higher in elevation compared to records from 210 years ago. [23] He also contributed to a related European study showing that the rate of increase in plant species richness on mountain summits in Europe has accelerated in recent decades,linked to climate warming. [24] With colleagues,he also determined that past defaunation has severely reduced plant migration rates,which could limit the ability of plant species to adapt to climate change. [25]
Through his work,Svenning emphasized that vegetation will likely experience disequilibrium with climate change,with marked changes at both leading and trailing edges. [26] In a study with Skov,he established that European tree species fill their climatically determined potential ranges by only 38%,suggesting limited tracking of near-future climate changes. [27] Later,together with Seliger,McGill and Gill,he determined that North American trees and shrubs are mostly not fully utilizing their potential climatic niches,with climate explaining only about half of the species' ranges,and small-ranged species showing high levels of climatic disequilibrium likely due to dispersal lags as well as undetected environmental factors or biotic interactions. [28] Additionally,he has contributed to work showing that warming-induced tree and shrub expansion within the Arctic will be limited by dispersal,soil development,and other disequilibrium dynamics,but plantings and unintentional seed dispersal by humans could have large impacts on spread rates. [29] Moreover,as part of a large team,he demonstrated that high-mountain plant species in the European Alps are projected to experience substantial range reductions of around 44-50% by the end of the twenty-first century,with population dynamics lagging behind climatic trends and creating an extinction debt,especially impacting species endemic to the Alps. [30]
Svenning also looked into human-megafauna interactions,megafauna extinctions in recent prehistory,and the ecological role of megafauna in shaping past and present ecosystems. In further collaborative research,he determined that cultural filtering has been the dominant driver of megafauna range contractions in China over the past 2 millennia. [31] With Faurby,he found that human activities have significantly altered Earth's mammal diversity patterns,leading to strong deviations in current patterns compared to their natural state for large-bodied species,emphasizing the need to consider natural distributions for a better understanding of diversity drivers and conservation benchmarks. [32]
More recently,in 2023,Svenning conducted a joint study with Lemoine and Buitenwerf and found that human impact had been the primary driver of late-Quaternary megafauna extinctions,outperforming climatic models. [33] In another collaborative study,he challenged the perception of recent human impact on terrestrial nature,revealing through that nearly three quarters of the Earth's land was inhabited and shaped by human societies over 12,000 years ago. [34] Linked to this work,he and colleagues established that the current rate of extinctions among mammals –across body sizes –suggested that the incipient sixth mass extinction will lead to the loss of a significant amount of phylogenetic diversity,which will take millions of years to recover even if extinction rates revert to pre-human levels. [35]
Furthermore,with colleagues,Svenning identified the presence of abundant and diverse large herbivores in Great Britain during the Last Interglacial period alongside high structural diversity in vegetation. [36] In an earlier review in 2002,he estimated that closed forests would have predominated in north-western Europe under existing natural conditions,but open vegetation would also be frequent in varied settings and maintained by large herbivores and fire. [37] In 2023,in work led by Pearce,he and colleagues showed based on extensive pollen records that substantial light woodland and open vegetation characterized the temperate forest biome in Europe during the Last Interglacial,suggesting the rich megafauna as a likely key driver of this structure. [38]
Svenning has studied rewilding and conservation. He has proposed that trophic rewilding via restoring top-down trophic interactions and associated trophic cascades is a promising strategy to promote self-regulating biodiverse ecosystems, [39] and that it could be a powerful tool for mitigating the impacts of human-induced global change on biodiversity and ecosystems. [40] With colleagues,he further provided a definition and guiding principles that clarify the concept for understanding of rewilding as a continuum of scale and human influence,emphasizing ecosystem restoration to achieve autonomous nature, [41] and emphasizing rewilding as a central approach to ecosystem restoration to promote ecological resilience. [42]
Svenning has explored globalization,alien species invasions and related issues such as biotic homogenization. In a study published in Nature,he and Fricke demonstrated that human-induced species introductions are leading to the homogenization of global ecological networks,diminishing beta diversity among local networks and modularity within networks,with potential consequences for ecosystem resilience and coevolutionary dynamics. [43]
In a joint study,Svenning revealed that human activities in China have caused narrow-ranged plant species to fill their climatic potential ranges to a lesser extent than widespread species,leading to a risk of biotic homogenization also among native species. [44]
In a collaborative study,Svenning highlighted the potential of megaherbivores in managing plant invasions and promoting native plant diversity,particularly in protected areas with high megaherbivore densities and mid-productive ecosystems,supporting the concept of trophic rewilding. [45]
Svenning's research in human ecology focuses on the history of environmental transformation and the relationship between human beings and the natural environment. In a joint study,he determined that childhood exposure to green spaces is linked to a reduced risk of a broad variety of psychiatric disorders later in life,underscoring the importance of incorporating natural environments into urban planning and childhood experiences for improved mental health. [46] As part of a team,he also found that climate change is shifting the human climate niche at an unprecedented rate,with potentially devastating consequences for the poorest regions of the world, [47] and that it could push one-third of humanity outside the human climate niche by end-of-century under current policies,but reducing warming to 1.5°C would limit exposure to unprecedented heat to 5%. [48]
Svenning has integrated use of remote sensing and ecoinformatics into his research to better understand ecological patterns and processes. In a collaborative research,with colleagues he showed that using a multilevel approach with satellite data can significantly enhance the prediction of household wealth in rural areas,aiding the monitoring of poverty-related Sustainable Development Goals (SDGs). [49] Together with colleagues,he has contributed to the development of several larger databases on biodiversity data such as PHYLACINE,which contained phylogenies,range maps,trait data,and threat status for all known mammal species,taking into account human impacts. [50] Additionally,jointly with his team he also developed the TREECHANGE database, [51] as well as the Botanical Information Ecology Network (BIEN) where ecologists,botanists and computer scientists assemble worldwide data on plant geographic distribution,diversity,and functionality. [52]
*Svenning, J. C., & Skov, F. (2004). Limited filling of the potential range in European tree species. Ecology Letters, 7(7), 565-573.
The Holocene extinction, or Anthropocene extinction, is the ongoing extinction event caused by humans during the Holocene epoch. These extinctions span numerous families of plants and animals, including mammals, birds, reptiles, amphibians, fish, and invertebrates, and affecting not just terrestrial species but also large sectors of marine life. With widespread degradation of biodiversity hotspots, such as coral reefs and rainforests, as well as other areas, the vast majority of these extinctions are thought to be undocumented, as the species are undiscovered at the time of their extinction, which goes unrecorded. The current rate of extinction of species is estimated at 100 to 1,000 times higher than natural background extinction rates and is increasing. During the past 100–200 years, biodiversity loss and species extinction have accelerated, to the point that most conservation biologists now believe that human activity has either produced a period of mass extinction, or is on the cusp of doing so. As such, after the "Big Five" mass extinctions, the Holocene extinction event has also been referred to as the sixth mass extinction or sixth extinction; given the recent recognition of the Capitanian mass extinction, the term seventh mass extinction has also been proposed for the Holocene extinction event.
Biodiversity is the variability of life on Earth. It can be measured on various levels. There is for example genetic variability, species diversity, ecosystem diversity and phylogenetic diversity. Diversity is not distributed evenly on Earth. It is greater in the tropics as a result of the warm climate and high primary productivity in the region near the equator. Tropical forest ecosystems cover less than one-fifth of Earth's terrestrial area and contain about 50% of the world's species. There are latitudinal gradients in species diversity for both marine and terrestrial taxa.
In zoology, megafauna are large animals. The precise definition of the term varies widely, though a common threshold is approximately 45 kilograms (99 lb), with other thresholds as low as 10 kilograms (22 lb) or as high as 1,000 kilograms (2,200 lb). Large body size is generally associated with other traits, such as having a slow rate of reproduction and, in large herbivores, reduced or negligible adult mortality from being killed by predators.
Habitat conservation is a management practice that seeks to conserve, protect and restore habitats and prevent species extinction, fragmentation or reduction in range. It is a priority of many groups that cannot be easily characterized in terms of any one ideology.
An apex predator, also known as a top predator or superpredator, is a predator at the top of a food chain, without natural predators of its own.
In biology, a refugium is a location which supports an isolated or relict population of a once more widespread species. This isolation (allopatry) can be due to climatic changes, geography, or human activities such as deforestation and overhunting.
Naturalisation is the ecological phenomenon through which a species, taxon, or population of exotic origin integrates into a given ecosystem, becoming capable of reproducing and growing in it, and proceeds to disseminate spontaneously. In some instances, the presence of a species in a given ecosystem is so ancient that it cannot be presupposed whether it is native or introduced.
Charismatic megafauna are animal species that are large—in the relevant category that they represent—with symbolic value or widespread popular appeal, and are often used by environmental activists to gain public support for environmentalist goals. In this definition, animals such as penguins or bald eagles can be considered megafauna because they are among the largest animals within the local animal community, and they disproportionately affect their environment. The vast majority of charismatic megafauna species are threatened and endangered by overhunting, poaching, black market trade, climate change, habitat destruction, invasive species, and many more causes. In a 2018 study, the top twenty most popular charismatic megafauna were found to be : the tiger, lion, elephant, giraffe, leopard, giant panda, cheetah, polar bear, wolf, gorilla, chimpanzee, zebra, hippopotamus, great white shark, crocodile, dolphin, rhinoceros, brown bear, koala and blue whale.
Soil ecology studies interactions among soil organisms, and their environment. It is particularly concerned with the cycling of nutrients, soil aggregate formation and soil biodiversity.
There are several plausible pathways that could lead to an increased extinction risk from climate change. Every plant and animal species has evolved to exist within a certain ecological niche. But climate change leads to changes of temperature and average weather patterns. These changes can push climatic conditions outside of the species' niche, and ultimately render it extinct. Normally, species faced with changing conditions can either adapt in place through microevolution or move to another habitat with suitable conditions. However, the speed of recent climate change is very fast. Due to this rapid change, for example Ectotherm cold-blooded animals may struggle to find a suitable habitat within 50 km of their current location at the end of this century.
The Late Pleistocene to the beginning of the Holocene saw the extinction of the majority of the world's megafauna, which resulted in a collapse in faunal density and diversity across the globe. The extinctions during the Late Pleistocene are differentiated from previous extinctions by its extreme size bias towards large animals, and widespread absence of ecological succession to replace these extinct megafaunal species, and the regime shift of previously established faunal relationships and habitats as a consequence. The timing and severity of the extinctions varied by region and are thought to have been driven by varying combinations of human and climatic factors. Human impact on megafauna populations is thought to have been driven by hunting ("overkill"), as well as possibly environmental alteration. The relative importance of human vs climatic factors in the extinctions has been the subject of long-running controversy.
There is an ongoing decline in plant biodiversity, just like there is ongoing biodiversity loss for many other life forms. One of the causes for this decline is climate change. Environmental conditions play a key role in defining the function and geographic distributions of plants. Therefore, when environmental conditions change, this can result in changes to biodiversity. The effects of climate change on plant biodiversity can be predicted by using various models, for example bioclimatic models.
Rewilding is a form of ecological restoration aimed at increasing biodiversity and restoring natural processes. It differs from other forms of ecological restoration in that rewilding aspires to reduce human influence on ecosystems. It is also distinct from other forms of restoration in that, while it places emphasis on recovering geographically specific sets of ecological interactions and functions that would have maintained ecosystems prior to human influence, rewilding is open to novel or emerging ecosystems which encompass new species and new interactions.
In ecology, the term productivity refers to the rate of generation of biomass in an ecosystem, usually expressed in units of mass per volume per unit of time, such as grams per square metre per day. The unit of mass can relate to dry matter or to the mass of generated carbon. The productivity of autotrophs, such as plants, is called primary productivity, while the productivity of heterotrophs, such as animals, is called secondary productivity.
Equus semplicatus was a Pleistocene species of New World stilt-legged horse, and considered the type species for the stilt legged horses, one of three lineages of equids within the Americas, the other two being hippidionid and caballine horses. Now extinct, Equus semiplicatus once inhabited North America.
Biodiversity loss happens when plant or animal species disappear completely from Earth (extinction) or when there is a decrease or disappearance of species in a specific area. Biodiversity loss means that there is a reduction in biological diversity in a given area. The decrease can be temporary or permanent. It is temporary if the damage that led to the loss is reversible in time, for example through ecological restoration. If this is not possible, then the decrease is permanent. The cause of most of the biodiversity loss is, generally speaking, human activities that push the planetary boundaries too far. These activities include habitat destruction and land use intensification. Further problem areas are air and water pollution, over-exploitation, invasive species and climate change.
Sandra Myrna DíazForMemRS is an Argentine ecologist and professor of ecology at the National University of Córdoba, who has been awarded with the Linnean Medal for her scientific work. She studies the functional traits of plants and investigates how plants impact the ecosystem.
The wood-pasture hypothesis is a scientific hypothesis positing that open and semi-open pastures and wood-pastures formed the predominant type of landscape in post-glacial temperate Europe, rather than the common belief of primeval forests. The hypothesis proposes that such a landscape would be formed and maintained by large wild herbivores. Although others, including landscape ecologist Oliver Rackham, had previously expressed similar ideas, it was the Dutch researcher Frans Vera, who, in his 2000 book Grazing Ecology and Forest History, first developed a comprehensive framework for such ideas and formulated them into a theorem. Vera's proposals, although highly controversial, came at a time when the role grazers played in woodlands was increasingly being reconsidered, and are credited for ushering in a period of increased reassessment and interdisciplinary research in European conservation theory and practice. Although Vera largely focused his research on the European situation, his findings could also be applied to other temperate ecological regions worldwide, especially the broadleaved ones.
Richard Simon Ostfeld is a Distinguished Senior Scientist at the Cary Institute of Ecosystem Studies in Millbrook, New York. He is best known for his work on the ecology of Lyme disease, which he began studying while monitoring the abundance of small mammals in the forests of Cary Institute property in the early 1990s.
Megaherbivores are large herbivores that can exceed 1,000 kg (2,200 lb) in weight. The earliest herbivores to reach such sizes like the parieasaurs appeared in the Permian period. During most of the Mesozoic, the megaherbivore niche was largely dominated by dinosaurs up until their extinction during the Cretaceous–Paleogene extinction event. After this period, small mammalian species evolved into large herbivores in the Paleogene. As part of the Late Pleistocene megafauna extinctions, 80% of megaherbivore species became extinct, with megaherbivores becoming entirely extinct in Europe, Australia and the Americas. Recent megaherbivores include elephants, rhinos, hippos, and giraffes. There are nine extant species of terrestrial megaherbivores living in Africa and Asia. The African bush elephant is the largest extant species.
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