Evaluating Trophic Rewilding As a Conservation Technique Aaron Sieve Augustana College, Rock Island Illinois
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Rewilding Watersheds: Using Nature's Algorithms to Fix Our Broken Rivers
Marine and Freshwater Research © CSIRO 2021 https://doi.org/10.1071/MF20335_AC Supplementary material Rewilding watersheds: using nature’s algorithms to fix our broken rivers Natalie K. RideoutA,G,1, Bernhard WegscheiderB,1, Matilda KattilakoskiA, Katie M. McGeeC,D, Wendy A. MonkE, and Donald J. BairdF ACanadian Rivers Institute, Department of Biology, University of New Brunswick, 10 Bailey Drive, Fredericton, NB, E3B 5A3, Canada. BCanadian Rivers Institute, Faculty of Forestry and Environmental Management, University of New Brunswick, 2 Bailey Drive, Fredericton, NB, E3B 5A3, Canada. CEnvironment and Climate Change Canada, Canada Centre for Inland Waters, 867 Lakeshore Road, Burlington, ON, L7R 4A6, Canada. DCentre for Biodiversity Genomics and Department of Integrative Biology, University of Guelph, 50 Stone Road E., Guelph, ON, N1G 2W1, Canada. EEnvironment and Climate Change Canada @ Canadian Rivers Institute, Faculty of Forestry and Environmental Management, University of New Brunswick, 2 Bailey Drive, Fredericton, NB, E3B 5A3, Canada. FEnvironment and Climate Change Canada @ Canadian Rivers Institute, Department of Biology, University of New Brunswick, 10 Bailey Drive, Fredericton, NB, E3B 5A3, Canada. GCorresponding author. Email: [email protected] 1These authors contributed equally to the work. Page 1 of 49 Table S1. References linking ecosystem functions with rewilding goals, providing supporting evidence for Fig. 1 Restore natural flow Mitigate climate Restore riparian Re-introduce Improve water quality Reduce habitat and sediment regime warming vegetation extirpated species fragmentation 1 Metabolism Aristi et al. 2014 Song et al. 2008 Wassenaar et al. 2010 Huang et al. 2018 Jankowski and Schindler 2019 2 Decomposition Delong 2010 Perry et al. 2011 Delong 2010 Wenisch et al. -
This Article Appeared in a Journal Published by Elsevier
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Science Reviews 57 (2012) 26e45 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Mammoth steppe: a high-productivity phenomenon S.A. Zimov a,*, N.S. Zimov a, A.N. Tikhonov b, F.S. Chapin III c a Northeast Science Station, Pacific Institute for Geography, Russian Academy of Sciences, Cherskii 678830, Russia b Zoological Institute, Russian Academy of Sciences, Saint Petersburg 199034, Russia c Institute of Arctic Biology, University of Alaska, Fairbanks, AK 99775, USA article info abstract Article history: At the last deglaciation Earth’s largest biome, mammoth-steppe, vanished. Without knowledge of the Received 11 January 2012 productivity of this ecosystem, the evolution of man and the glacialeinterglacial dynamics of carbon Received in revised form storage in Earth’s main carbon reservoirs cannot be fully understood. -
Rewilding North America Set Aside to Become the Would See the Introduction of Giant Introduction of Giant Wilderness Again
Focus: Brave New World REWILDING NORTH One elephant AMERICA at a By Alexandra Mushegian round sloths occupy a small but was the major cause of these extinctions. time Gbeloved role in the collective Without exception, the timing of major imagination. These five-ton, seventeen- biodiversity reductions on all continents foot hamster-like herbivores, which and large islands coincides with the ar- went extinct somewhere around 10,000 rival of early humans, with many species years ago, are commonly found as dying out within a few hundred years skeletons posing in natural history mu- after humans arrived (1). seums. Populations of these animals The only continents still possessing were thriving in North America when noteworthy megafaunal diversity— humans first arrived over the Bering Africa, and to a lesser extent, Asia—are Land Bridge along with mammoths, the continents where humans coevolved lions, saber-toothed cats, twenty-pound with animals for the longest time. Now, beavers, and several species of giant due to political and socioeco- tortoise, not to mention a multitude of nomic instability in those deer and ox-like species. Shortly after regions, they are in danger humans arrived, they all died out. there too. The Pleistocene epoch, which ended Some scientists believe 10,000 years ago (in archaeological that the loss of large ver- terms, the end of the Paleolithic), was tebrate biodiversity has a golden age of animal exoticism world- graver consequences than wide. Why it ended—why this geologi- merely a reduction in worldwide cal period saw a series of massive global biodiversity. Ecological studies suggest collapses of large animal biodiversity— that large herbivores and predators are is a contentious topic. -
Pleistocene Park
Welcome to Pleistocene Park Welcome to Pleistocene Park In Arctic Siberia, Russian scientists are working to turn back time by resurrecting an Ice Age environment complete with lab- grown woolly mammoths. Pleistocene Park is a radical geoengineering scheme whose goal is to combat climate change. It’s named for the geological epoch often known as the Ice Age, which ended 12,000 years ago. At that time, huge sections of the earth were covered in grasslands. When the Ice Age ended, many of the grasslands disappeared, along with most of the giant species who called them home. The purpose of Pleistocene Park is to slow the thawing of the permafrost. Research suggests that grasslands reflect more sunlight than forests, which causes the Arctic to absorb less heat. In winter, the short grass enables the season’s freeze to extend deeper into the Earth’s crust, cooling the frozen soil. Large herbivores are needed to test these landscape-cooling effects. While Pleistocene Park is currently home to bison, musk oxen and wild horses, hundreds of thousands of woolly mammoths are necessary to keep the trees back. Mammoths are cold-adapted members of the elephant family. Geneticist George Church is working on editing the genomes of Asian elephants and switching in mammoth traits. In 2016, he had succeeded in editing 45 of the Asian elephant’s genes, and he hopes to deliver the first woolly mammoth to Pleistocene Park within a decade. While it might seem like the stuff of mythology, Pleistocene Park provides us with the chance to bring another era back to the Arctic and may even have a shot at saving the planet. -
Prospects for Rewilding with Camelids
Journal of Arid Environments 130 (2016) 54e61 Contents lists available at ScienceDirect Journal of Arid Environments journal homepage: www.elsevier.com/locate/jaridenv Prospects for rewilding with camelids Meredith Root-Bernstein a, b, *, Jens-Christian Svenning a a Section for Ecoinformatics & Biodiversity, Department of Bioscience, Aarhus University, Aarhus, Denmark b Institute for Ecology and Biodiversity, Santiago, Chile article info abstract Article history: The wild camelids wild Bactrian camel (Camelus ferus), guanaco (Lama guanicoe), and vicuna~ (Vicugna Received 12 August 2015 vicugna) as well as their domestic relatives llama (Lama glama), alpaca (Vicugna pacos), dromedary Received in revised form (Camelus dromedarius) and domestic Bactrian camel (Camelus bactrianus) may be good candidates for 20 November 2015 rewilding, either as proxy species for extinct camelids or other herbivores, or as reintroductions to their Accepted 23 March 2016 former ranges. Camels were among the first species recommended for Pleistocene rewilding. Camelids have been abundant and widely distributed since the mid-Cenozoic and were among the first species recommended for Pleistocene rewilding. They show a range of adaptations to dry and marginal habitats, keywords: Camelids and have been found in deserts, grasslands and savannas throughout paleohistory. Camelids have also Camel developed close relationships with pastoralist and farming cultures wherever they occur. We review the Guanaco evolutionary and paleoecological history of extinct and extant camelids, and then discuss their potential Llama ecological roles within rewilding projects for deserts, grasslands and savannas. The functional ecosystem Rewilding ecology of camelids has not been well researched, and we highlight functions that camelids are likely to Vicuna~ have, but which require further study. -
Donlan CJ. 2007. Restoring America's Big Wild Animals
Donlan CJ. 2007. Restoring America's big wild animals. Scientific American June 2007:72-7. Keywords: 1NAm/cheetah/cougar/jaguar/lion/megafauna/Miracinonyx trumani/Panthera leo/Panthera onca/Pleistocene/Puma concolor/saber-toothed cat Abstract: Pleistocene rewilding-a proposal to bring back animals that disappeared from North America 13,000 years ago-offers an optimistic agenda for 21st-century conservation. In the fall of 2004 a dozen conservation biologists gathered on a ranch in New Mexico to ponder a bold plan. The scientists, trained in a variety of disciplines, ranged from the grand old men of the fi eld to those of us earlier in our careers. The idea we were mulling over was the reintroduction of large vertebrates-megafauna-to North America. Most of these animals, such as mammoths and cheetahs, died out roughly 13,000 years ago, when humans from Eurasia began migrating to the continent. The theory-propounded 40 years ago by Paul Martin of the University of Arizona- is that overhunting by the new arrivals reduced the numbers of large vertebrates so severely that the populations could not recover. Called Pleistocene overkill, the concept was highly controversial at the time, but the general thesis that humans played a significant role is now widely accepted. Martin was present at the meeting in New Mexico, and his ideas on the loss of these animals, the ecological consequences, and what we should do about it formed the foundation of the proposal that emerged, which we dubbed Pleistocene rewilding. Restoring America’s n the fall of 2004 a dozen conservation biologists gath- Although the cheetahs, lions and mammoths that once ered on a ranch in New Mexico to ponder a bold plan. -
Effects of Large Herbivore Grazing on Relics of the Presumed Mammoth
www.nature.com/scientificreports OPEN Efects of large herbivore grazing on relics of the presumed mammoth steppe in the extreme climate of NE‑Siberia Jennifer Reinecke1,2*, Kseniia Ashastina3,4, Frank Kienast3, Elena Troeva5 & Karsten Wesche1,2,6 The Siberian mammoth steppe ecosystem changed dramatically with the disappearance of large grazers in the Holocene. The concept of Pleistocene rewilding is based on the idea that large herbivore grazing signifcantly alters plant communities and can be employed to recreate lost ecosystems. On the other hand, modern rangeland ecology emphasizes the often overriding importance of harsh climates. We visited two rewilding projects and three rangeland regions, sampling a total of 210 vegetation relevés in steppe and surrounding vegetation (grasslands, shrublands and forests) along an extensive climatic gradient across Yakutia, Russia. We analyzed species composition, plant traits, diversity indices and vegetation productivity, using partial canonical correspondence and redundancy analysis. Macroclimate was most important for vegetation composition, and microclimate for the occurrence of extrazonal steppes. Macroclimate and soil conditions mainly determined productivity of vegetation. Bison grazing was responsible for small‑scale changes in vegetation through trampling, wallowing and debarking, thus creating more open and disturbed plant communities, soil compaction and xerophytization. However, the magnitude of efects depended on density and type of grazers as well as on interactions with climate and site conditions. Efects of bison grazing were strongest in the continental climate of Central Yakutia, and steppes were generally less afected than meadows. We conclude that contemporary grazing overall has rather limited efects on vegetation in northeastern Siberia. Current rewilding practices are still far from recreating a mammoth steppe, although large herbivores like bison can create more open and drier vegetation and increase nutrient availability in particular in the more continental Central Yakutian Plain. -
Environmental Protection / Species Preservation
The projest has been funded with the support of European Commission within ERASMUS+ program Rewilding as a way of preserving ecosystem Material for students This work is licensed under a Creative Commons Attribution 4.0 International License(CC BY 4.0). This material has been founded with support from the European Commission. This publication reflects the views only of the author, and the Commission cannot be held responsible for any use which may be made of the information contained therein. Publication free of charge. Project office: Ks. Janusza 64, 01‐452, Warsaw, Polandhttp://[email protected] The projest has been funded with the support of European Commission within ERASMUS+ program Introduction Resolution The best way to preserve an ecosystem is by rewilding. Definitions Trophic cascades Predators feed on their prey. By doing so, predators can influence the abundance and behavior of prey. In other words, prey abundance can be reduced if there are predators nearby, or prey can hide or move further. When the influence of a predator on its prey is so large that it reduces the trophic level at anotherlevel of the food chain affecting the density and/or behavior of prey, ecologists call this interaction a trophic cascade. For a long time, the prevailing ecological theory was the one stating that climate and local resources control species distribution and primary production in ecosystems ‐ the level of organic ingredients in an ecosystem produced by plants and other photosynthetic organisms. Since the world is rich in vegetation, the effect of unstoppable consumption of plants was considered an exception and was seen as a relatively insignificant factor. -
Synthesis and Future Directions for Trophic Rewilding Research Jens-Christian Svenninga,1,2,Pilb.M.Pedersena,1, C
SPECIAL FEATURE: PERSPECTIVE PERSPECTIVE SPECIAL FEATURE: Science for a wilder Anthropocene: Synthesis and future directions for trophic rewilding research Jens-Christian Svenninga,1,2,PilB.M.Pedersena,1, C. Josh Donlanb,c, Rasmus Ejrnæsd, Søren Faurbya,MauroGalettie, Dennis M. Hansenf, Brody Sandela, Christopher J. Sandomg, John W. Terborghh, and Frans W. M. Verai aSection for Ecoinformatics & Biodiversity, Department of Bioscience, Aarhus University, DK-8000 Aarhus C, Denmark; bAdvanced Conservation Strategies, Midway, UT 84049; cDepartment of Ecology and Evolutionary Biology, Cornell University, Ithaca, NY 15853; dSection for Biodiversity & Conservation, Department of Bioscience, Aarhus University, DK-8410 Rønde, Denmark; eDepartamento de Ecologia, Universidade Estadual Paulista, 13506-900 Rio Claro, São Paulo, Brazil; fInstitute of Evolutionary Biology and Environmental Studies, University of Zurich, 8057 Zurich, Switzerland; gWildlife Conservation Research Unit, Department of Zoology, Oxford University, The Recanati-Kaplan Centre, Oxfordshire OX13 5QL, United Kingdom; hCenter for Tropical Conservation, Nicholas School of the Environment and Earth Sciences, Duke University, Durham, NC 27708; and iCommunity and Conservation Ecology, Groningen Institute for Evolutionary Life Sciences, University of Groningen, Cocon, 9700 CC Groningen, The Netherlands Edited by Yadvinder Malhi, Oxford University, Oxford, United Kingdom, and accepted by the Editorial Board August 5, 2015 (received for review March 16, 2015) Trophic rewilding is an ecological restoration strategy that uses species introductions to restore top-down trophic interactions and associated trophic cascades to promote self-regulating biodiverse ecosystems. Given the importance of large animals in trophic cascades and their widespread losses and resulting trophic downgrading, it often focuses on restoring functional megafaunas. Trophic rewilding is increasingly being implemented for conservation, but remains controversial. -
Climate Geoengineering Options: Practical, Powerful, and to Be Avoided If Possible Report on the 2Nd Permafrost Carbon Feedback Intervention Roadmap Dialogue
AVOIDING PERMAFROST THAW: MANAGING TEMPERATURE Climate geoengineering options: practical, powerful, and to be avoided if possible Report on the 2nd Permafrost Carbon Feedback Intervention Roadmap Dialogue To avoid catastrophic risk from climate change, we need to limit global warming to 1.5° Celsius. And given how close we are to that limit, even the most ambitious conventional decarbonization efforts will not be enough. Negative-emission technologies or other geoengineering methods will be necessary to compensate for emissions that push us beyond that manageable limit. That statement, paraphrased from Leiden University researcher and guest presenter Oscar Rueda, probably best captures the consensus of a sometimes-fractious second dialogue (March 11, 2021) facilitated by the privately sponsored Permafrost Carbon Feedback Action Group – part of a four-session virtual symposia addressing the science, technology, economics, policy, social and ethical implications of permafrost thaw. The first dialogue (March 4, 2021) surveyed Why Permafrost Carbon Matters and garnered easy agreement: global permafrost is charged with twice as much carbon as that in all the earth’s atmosphere and, as it thaws, natural processes trigger a dangerous release of that carbon in the form of the greenhouse gases CO2 and methane, thereby reinforcing atmospheric warming. The second dialogue, Avoiding Permafrost Thaw: Managing Temperature, considered whether we have the capacity to intervene to limit permafrost thaw – and whether we should. Even the first question provoked argument. The second, however, inspired a fiercer debate, among panelists and among more than 150 leading academics, government policy makers, technology investors, climate change activists and media who had tuned in online. -
Targeted Geoengineering: Conserving the Cryosphere
Targeted Geoengineering: Conserving the Cryosphere Permafrost conservation through land-use modification - are potential solutions practicable and scalable? John Moore Photo T. Kumpula Mitigation The 3 standard Adaptation paradigms Solar Geoengineering Can anything else be done? • In some cases Targeted Geoengineering might provide partial solutions • Land surface albedo: Pleistocene Park in Siberia for permafrost • Arctic ice management for sea ice • Glacier geoengineering for sea level – by far the most realistic Pleistocene Park Courtesy N. Zimov www. https://pleistocenepark.ru/ Courtesy N. Zimov www. https://pleistocenepark.ru/ Courtesy N. Zimov www. https://pleistocenepark.ru/ The albedo of the steppe grassland is much higher than the forest or shrub lands, especially in winter Hence the Permafrost is cooler Courtesy N. Zimov www. https://pleistocenepark.ru/ Pleistocene Park Courtesy N. Zimov www. https://pleistocenepark.ru/ Pleistocene Park Target MEG density. Assuming that animal density in the mammoth steppe can be estimated from the number of bones found in the permafrost, an estimated average of 1 mammoth, 5 bison, 7.5 horses, 15 reindeer, 0.25 cave lions, and 1 wolf per 1km2 1 MEG costs $383,000 MEG growth rate. 10% / yr Assuming a constant animal introduction rate of 10 MEG/yr after 30 years, an area of 3100 km2 would be converted to grassland. 0.03% of permafrost area Conversion of 1 million km2 of Arctic tundra (10% of the Arctic permafrost zone) in 30 years would require an introduction rate of 7,000 MEGs /yr which is unrealistic. Pleistocene Park Target MEG density. Assuming that animal density in the mammoth steppe can be estimated from the number of bones found in the permafrost, an estimated average of 1 mammoth, 5 bison, 7.5 horses, 15 reindeer, 0.25 cave lions, and 1 wolf per 1km2 1 MEG costs $383,000 MEG growth rate. -
Arctic Viewpoints to the Governance of Climate-Altering Approaches
Arctic viewpoints to the governance of climate-altering approaches C2GLearn: Climate-altering approaches and the Arctic Visiting researcher Ilona Mettiäinen M.Sc., PhD Candidate Arctic Centre, University of Lapland What is governance? • IPCC 2018: ”a comprehensive and inclusive concept of the full range of means for deciding, managing, implementing and monitoring policies and measures” • Many levels from local to global; multilevel governance • Governments, scientific community, media, business, civil society • Rules, regulations and laws; international cooperation; market instruments; incentives, funding and support; guidelines and codes of conduct; unwritten norms The Arctic as a region • The Arctic is a home to 4-4,5 million inhabitants • 8 countries and several indigenous peoples • 10-20 % indigenous population • The Arctic has <0,05 % of the global population (7,4 billion) The Arctic Portal Google Image Search 5.9.2020 All photos on this slide © Ilona Mettiäinen ”What happens in the Arctic doesn’t stay in the Arctic” • The Arctic is warming 2-3 times faster than the global average • The impacts of climate change are seen first in the Arctic • Keeping the global warming at 1.5 degrees would help to alleviate or avoid some negative impacts, but that would still mean 5,5 degrees warming in the Arctic (NASA) • Several tipping points in the Arctic with global consequences • Melting of the Greenland ice sheet can cause several meters’ sea level rise • Saving the Arctic by climate-altering techniques for the Arctic or for global reasons?