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The Cary Institute of Ecosystem Studies , formerly known as the Institute of Ecosystem Studies, is an independent, not-for-profit environmental research organization dedicated to the scientific study of the world’s ecosystems and the natural and human factors that influence them. Research is communicated in scholarly publications for scientific peers, educational programs for students and public audiences, and focused outreach to elected officials, policy makers, and the media.Located in Millbrook, New York , at the 2,000-acre Mary Flagler Cary Arboretum, the Cary Institute has about 120 employees, of which about 20 are scientists with Ph.D.’s in ecology and allied fields. While the Cary Institute is not itself a degree-granting institution, numerous graduate students are trained under the mentorship of the scientific staff who have adjunct appointments at many universities. The Cary Institute has hosted research experiences for undergraduates since 1987.The Cary Institute is organized as a 501c3 corporation with financial support from multiple sources which include the Mary Flagler Charitable Trust, research and education grants from federal and state sources , private foundations, and private donors. Wikipedia.

Lovett G.M.,Cary Institute of Ecosystem Studies
Annals of the New York Academy of Sciences | Year: 2013

Repeated invasions of non-native insects and pathogens have altered the structure and function of forest ecosystems in the Catskill Mountains of New York State, and will continue to do so in the future. Gypsy moth, beech bark disease, and hemlock woolly adelgid are among the insects and diseases currently established in the Catskills that are having significant effects on forests. Many others, including emerald ash borer, Asian long-horned beetle, Phytophthora ramorum, and Sirex wood wasp, are either very recently established in the Catskills or have been found elsewhere in North America and threaten to spread to this region. Short-term disturbances associated with these pests include reduction of productivity, tree decline and mortality, disruption of nutrient cycles, and reduction of seed production. Longer-term impacts are associated with shifts in tree species composition that alter productivity, nutrient cycling, and biodiversity. Catskill forests at mid to high elevations, such as the New York State Forest Preserve lands, are dominated by sugar maple and are particularly vulnerable to pests that use maple as a host, including the Asian long-horned beetle. The simultaneous effects of multiple invading insects and pathogens, and their interactions with changing climate and air pollution regimes, make it very difficult to predict the future composition of Catskill forests. © 2013 New York Academy of Sciences. Source

Likens G.E.,Cary Institute of Ecosystem Studies
Frontiers in Ecology and the Environment | Year: 2010

To guide environmental policy effectively, scientists face the difficult but crucial task of clearly communicating evidence-based information to the public and to policy makers. Frequently, the solutions proposed by scientists are hindered by poor communication - including an excessive reliance on acronyms and jargon - as well as being confronted by vested interests, both perceived and real. Although environmental "problems" are typically discovered by scientists, it is the media that often plays the primary role in promoting public awareness of - and political action regarding - such problems. Here, acid rain is used as a case study to illustrate many of the challenges commonly associated with environmental problems, including the long delay between initial discovery and relevant policy making. Some simple, straightforward recommendations are provided for facilitating communication about environmental problems. © The Ecological Society of America. Source

Jones C.G.,Cary Institute of Ecosystem Studies
Geomorphology | Year: 2012

Biogeomorphologists study the roles of biota in landscape formation and decay. Ecologists interested in ecosystem engineering study environmental change caused by biota and the consequences for the engineer, other organisms, and ecological processes. The interface is geomorphological change, an interface both are aware of but study somewhat independently and differently. Interaction and integration among the two fields is the goal of this special issue. Here I take an ecological perspective of geomorphological change caused by ecosystem engineers in patches within landscapes that I hope can help facilitate this goal. I ask the following general questions: When will an ecosystem engineering species create a geomorphological signature in a landscape? What, in qualitative terms, is such a signature? How can the signature be estimated and how long will it last? What engineer attributes and ecological factors will determine signature change? What creates complications? How do the answers inform whether or not life leaves a geomorphological signature? To attempt answers, I develop a provisional, general theory of ecosystem engineering signatures that draws on and integrates a geomorphological foundation of balance between formation and decay; landscape patch dynamics; a general framework for ecosystem engineering; and empirical studies. I treat a landscape engineering signature as the balance of rates of formation (F) and rates of decay (D) across patches whose ratio value (F/D) can be transformed (> 1), intermediate (1) or untransformed (< 1). I suggest amenable systems for study. I describe how the signature can be estimated and evaluated for potential persistence, and how to identify when decay or engineer density and per capita engineering activity control the signature. I examine the influences on shifts from transformed to untransformed signatures, and vice versa, at constant and changing rates of decay. I show how the likelihood of signature shifts depends on: 1. engineer density in the landscape and per patch; 2. per capita engineering activity as structure per patch and patches per engineer, or its contribution for engineers occurring in groups; 3. the degree of patch maintenance, abandonment, and re-engineering of abandoned patches; and in some situations, 4. the direction of the signature shift that is considered. I use this to illustrate how different ecological factors affecting engineer species (e.g., abiotic resources and conditions, natural enemies) and engineer feedbacks can drive signature transitions. I address complications and how they might be dealt with for situations where an engineer species causes formation and decay; when multiple engineering species co-occur; and when patches are materially interconnected. I end by considering whether life leaves a geomorphological signature, using this to contrast my approach with biogeomorphology, and asking what a hypothetical analysis of signature patterns across many engineer species/landscape combinations might imply for the interface of ecology and biogeomorphology. © 2011 Elsevier B.V. Source

Ostfeld R.S.,Cary Institute of Ecosystem Studies | Brunner J.L.,Washington State University
Philosophical Transactions of the Royal Society B: Biological Sciences | Year: 2015

The evidence that climate warming is changing the distribution of Ixodes ticks and the pathogens they transmit is reviewed and evaluated. The primary approaches are either phenomenological, which typically assume that climate alone limits current and future distributions, or mechanistic, asking which tick-demographic parameters are affected by specific abiotic conditions. Both approaches have promise but are severely limited when applied separately. For instance, phenomenological approaches (e.g. climate envelope models) often select abiotic variables arbitrarily and produce results that can be hard to interpret biologically. On the other hand, although laboratory studies demonstrate strict temperature and humidity thresholds for tick survival, these limits rarely apply to field situations. Similarly, no studies address the influence of abiotic conditions on more than a few life stages, transitions or demographic processes, preventing comprehensive assessments. Nevertheless, despite their divergent approaches, bothmechanistic and phenomenologicalmodels suggest dramatic range expansions of Ixodes ticks and tick-borne disease as the climate warms. The predicted distributions, however, vary strongly with the models’ assumptions, which are rarely tested against reasonable alternatives. These inconsistencies, limited data about key tick-demographic and climatic processes and only limited incorporation of non-climatic processes have weakened the application of this rich area of research to public health policy or actions. We urge further investigation of the influence of climate on vertebrate hosts and tick-borne pathogen dynamics. In addition, testing model assumptions and mechanisms in a range of natural contexts and comparing their relative importance as competing models in a rigorous statistical framework will significantly advance our understanding of how climate change will alter the distribution, dynamics and risk of tick-borne disease. © 2015 The Author(s) Published by the Royal Society. All rights reserved. Source

Schlesinger W.H.,Cary Institute of Ecosystem Studies
Global Change Biology | Year: 2010

Applications of fertilizer, often thought to enhance carbon sequestration in agricultural soils, are of no value to the mitigation of climate change if the carbon dioxide released during the production and distribution of nitrogen fertilizer exceeds the incremental carbon storage in soils from its use. Nitrogen fertilizer is also a source of the greenhouse gas nitrous oxide. The recent analysis of carbon sequestration in cropland soils of China does not apply these 'discounts' to the global warming mitigation expected from greater use of fertilizer; doing so would likely eliminate all the climate benefits of the postulated enhanced carbon sequestration. © 2009 Blackwell Publishing Ltd. Source

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