Principles of Terrestrial Ecosystem Ecology

By Stuart Chapin, P. Matson, Harold A. Mooney, Melissa C. Chapin. Springer: New York, 2002

3,656 citations recorded by the source corpus.

Subfields: Education, Management, Monitoring, Policy and Law

View Paper: https://www.semanticscholar.org/paper/3d73cfb71b0bb32fc94b186a16e9c24228a30ed4

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Education

1. David Tilman
2. Sean Schaeffer
3. J. Schimel
4. Jiquan Chen

In Management, Monitoring, Policy and Law

1. Yongfei Bai
2. Barbara C. Schmid
3. Daniel Müller
4. A. Wilby
5. Michel Loreau
6. C. Kremen
7. W. Bond
8. David Tilman

Citations in the corpus

• Microbial stress-response physiology and its implications for ecosystem function. (2007, positive): “Developing the full flow of the linkage between environment and processes via physiology and community composition has been a major theme in plant ecology over the last decade or more (Chapin et al. 2002).”
• Global resorption efficiencies and concentrations of carbon and nutrients in leaves of terrestrial plants (2012, background): “The availability of P and cations typically decline in old highly weathered soils, as they have been leached out of the system or become bound in unavailable forms (Vitousek and Sanford 1986, Chapin et al. 2011).”
• Erratum to The chemical and functional characterization of soil N and its biotic components (2009, background): “2) due to the activity of enzymes, such as extracellular proteases released by microorganisms (Chapin et al., 2002).”
• Mycorrhizal mediation of plant N acquisition and residue decomposition: Impact of mineral N inputs (2006, background): “Human activities have significantly increased N inputs to terrestrial ecosystems through mineral N fertilization and atmospheric N deposition, modifying the global N cycle (Chapin et al., 2002).”
• Soil Compaction, Corn Yield Response, and Soil Nutrient Pool Dynamics within an Integrated Crop-Livestock System in Illinois (2008, background): “Total C and N closely reflect quantity of soil organic matter and microbial biomass C is an active pool of organic matter whose size and activity strongly influences nutrient availability and plant productivity (Paul, 1984, Chapin et al. 2002).”
• Nitrous oxide emissions from soils: how well do we understand the processes and their controls? (2013, background): “The remaining unexplained gas fluxes are related to proximal drivers of oxygen supply, for example, substrate concentration, available energy and distal drivers of plant nitrate uptake, for example, litter/soil organic matter quality, root/microbial respiration, soil texture, predation, pH and pollu”
• EFFECTS OF BIODIVERSITY ON ECOSYSTEM FUNCTIONING: A CONSENSUS OF CURRENT KNOWLEDGE (2005, background): “1; Chapin et al. 1997, 2000, 2002, Lavorel and Garnier 2002).”
• Soil biota accelerate decomposition in high‐elevation forests by specializing in the breakdown of litter produced by the plant species above them (2009, background): “In part, this may have been caused by greater soil temperature in aspen stands and greater soil moisture in spruce stands, both of which are known to influence decomposition rates (Russell & Voroney 1998; Chapin, Matson & Mooney 2002; Hobbie et al. 2006).”
• Carbon storage in permafrost and soils of the mammoth tundra‐steppe biome: Role in the global carbon budget (2009, background): “For all scenarios, SCI is divided into 3 components: ‘‘very fast’’ (sugar, protein), 30% of total SCI; ‘‘fast’’ (labile: cellulose, hemicellulose), 45%; and ‘‘slow’’ (non-labile: lignin), 25% [Chapin et al., 2002].”
• Ecohydrological advances and applications in plant-water relations research: a review (2011, background): “On the other hand, plants are a primary conduit for returning terrestrial water to the atmosphere (Chapin et al. 2002) while mediating albedo and roughness (Pielke et al.”
• Stand age and soils as drivers of plant functional traits and aboveground biomass in secondary tropical dry forest (2014, background): “Carbon in biomass is generally expected to increase logistically as forests recover from disturbance (Chapin et al. 2011), but the maximum level of biomass reached and the time it takes to reach it can vary across the landscape (Turner 2010).”
• N fertilization affects on soil respiration, microbial biomass and root respiration in Larix gmelinii and Fraxinus mandshurica plantations in China (2010, positive): “It is known that N fertilization may lead to soil acidification (Chapin et al. 2002).”
• Does agricultural crop diversity enhance soil microbial biomass and organic matter dynamics? A meta-analysis. (2014, background): “Both MAT and MAP are strongly correlated with NPP and the overall quantity of SOM inputs (Chapin et al. 2002), which are directly related to soil C and N concentrations and microbial biomass (Raich and Schlesinger 1992, Wardle 1992, Amundson et al. 2003, Fierer et al. 2009).”
• Convergence across biomes to a common rain-use efficiency (2004, background): “However, both in locations with high MAP and in those with low MAP, water availability is tightly linked to biogeochemical constraints through mineralization processes and leachin”