Antoninka Plant and Soil 2017.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Long-Term Changes in Biological Soil Crust Cover and Composition Eva Dettweiler-Robinson1*, Jeanne M Ponzetti2 and Jonathan D Bakker3
Dettweiler-Robinson et al. Ecological Processes 2013, 2:5 http://www.ecologicalprocesses.com/content/2/1/5 RESEARCH Open Access Long-term changes in biological soil crust cover and composition Eva Dettweiler-Robinson1*, Jeanne M Ponzetti2 and Jonathan D Bakker3 Abstract Introduction: Communities change over time due to disturbances, variations in climate, and species invasions. Biological soil crust communities are important because they contribute to erosion control and nutrient cycling. Crust types may respond differently to changes in environmental conditions: single-celled organisms and bryophytes quickly recover after a disturbance, while lichens are slow growing and dominate favorable sites. Community change in crusts has seldom been assessed using repeated measures. For this study, we hypothesized that changes in crust composition were related to disturbance, topographic position, and invasive vegetation. Methods: We monitored permanent plots in the Columbia Basin in 1999 and 2010 and compared changes in crust composition, cover, richness, and turnover with predictor variables of herbivore exclosure, elevation, heat load index, time since fire, presence of an invasive grass, and change in cover of the invasive grass. Results: Bryophytes were cosmopolitan with high cover. Dominant lichens did not change dramatically. Indicator taxa differed by monitoring year. Bryophyte and total crust cover declined, and there was lower turnover outside of herbivore exclosures. Lichen cover did not change significantly. Plots that burned recently had high turnover. Increase in taxon richness was correlated with presence of an invasive grass in 1999. Change in cover of the invasive grass was positively related to proportional loss and negatively related to gain. Conclusions: Composition and turnover metrics differed significantly over 11 years, though cover was more stable between years. -
Agricultural Soil Compaction: Causes and Management
October 2010 Agdex 510-1 Agricultural Soil Compaction: Causes and Management oil compaction can be a serious and unnecessary soil aggregates, which has a negative affect on soil S form of soil degradation that can result in increased aggregate structure. soil erosion and decreased crop production. Soil compaction can have a number of negative effects on Compaction of soil is the compression of soil particles into soil quality and crop production including the following: a smaller volume, which reduces the size of pore space available for air and water. Most soils are composed of • causes soil pore spaces to become smaller about 50 per cent solids (sand, silt, clay and organic • reduces water infiltration rate into soil matter) and about 50 per cent pore spaces. • decreases the rate that water will penetrate into the soil root zone and subsoil • increases the potential for surface Compaction concerns water ponding, water runoff, surface soil waterlogging and soil erosion Soil compaction can impair water Soil compaction infiltration into soil, crop emergence, • reduces the ability of a soil to hold root penetration and crop nutrient and can be a serious water and air, which are necessary for water uptake, all of which result in form of soil plant root growth and function depressed crop yield. • reduces crop emergence as a result of soil crusting Human-induced compaction of degradation. • impedes root growth and limits the agricultural soil can be the result of using volume of soil explored by roots tillage equipment during soil cultivation or result from the heavy weight of field equipment. • limits soil exploration by roots and Compacted soils can also be the result of natural soil- decreases the ability of crops to take up nutrients and forming processes. -
Biological Soil Crust Community Types Differ in Key Ecological Functions
UC Riverside UC Riverside Previously Published Works Title Biological soil crust community types differ in key ecological functions Permalink https://escholarship.org/uc/item/2cs0f55w Authors Pietrasiak, Nicole David Lam Jeffrey R. Johansen et al. Publication Date 2013-10-01 DOI 10.1016/j.soilbio.2013.05.011 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Soil Biology & Biochemistry 65 (2013) 168e171 Contents lists available at SciVerse ScienceDirect Soil Biology & Biochemistry journal homepage: www.elsevier.com/locate/soilbio Short communication Biological soil crust community types differ in key ecological functions Nicole Pietrasiak a,*, John U. Regus b, Jeffrey R. Johansen c,e, David Lam a, Joel L. Sachs b, Louis S. Santiago d a University of California, Riverside, Soil and Water Sciences Program, Department of Environmental Sciences, 2258 Geology Building, Riverside, CA 92521, USA b University of California, Riverside, Department of Biology, University of California, Riverside, CA 92521, USA c Biology Department, John Carroll University, 1 John Carroll Blvd., University Heights, OH 44118, USA d University of California, Riverside, Botany & Plant Sciences Department, 3113 Bachelor Hall, Riverside, CA 92521, USA e Department of Botany, Faculty of Science, University of South Bohemia, Branisovska 31, 370 05 Ceske Budejovice, Czech Republic article info abstract Article history: Soil stability, nitrogen and carbon fixation were assessed for eight biological soil crust community types Received 22 February 2013 within a Mojave Desert wilderness site. Cyanolichen crust outperformed all other crusts in multi- Received in revised form functionality whereas incipient crust had the poorest performance. A finely divided classification of 17 May 2013 biological soil crust communities improves estimation of ecosystem function and strengthens the Accepted 18 May 2013 accuracy of landscape-scale assessments. -
Anatomy of a Sub-Cambrian Paleosol in Wisconsin
Anatomy of a Sub-Cambrian Paleosol in Wisconsin: Mass Fluxes of Chemical Weathering and Climatic Conditions in North America during Formation of the Cambrian Great Unconformity L. Gordon Medaris Jr.,1,* Steven G. Driese,2 Gary E. Stinchcomb,3 John H. Fournelle,1 Seungyeol Lee,1,4 Huifang Xu,1,4 Lyndsay DiPietro,2 Phillip Gopon,5 and Esther K. Stewart6 1. Department of Geoscience, University of Wisconsin, Madison, Wisconsin 53706, USA; 2. Department of Geosciences, Terrestrial Paleoclimatology Research Group, Baylor University, Waco, Texas 76798, USA; 3. Department of Geosciences and Watershed Studies Institute, Murray State University, Murray, Kentucky 42071, USA; 4. NASA Astrobiology Institute, University of Wisconsin, Madison, Wisconsin 53706, USA; 5. Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom; 6. Wisconsin Geological and Natural History Survey, Madison, Wisconsin 53705, USA ABSTRACT A paleosol beneath the Upper Cambrian Mount Simon Sandstone in Wisconsin provides an opportunity to evaluate the characteristics of Cambrian weathering in a subtropical climate, having been located at 207S paleolatitude 500 My ago. The 285-cm-thick paleosol resulted from advanced chemical weathering of a gabbroic protolith, recording a total mass loss of 50%. Weathering of hornblende and plagioclase produced a pedogenic assemblage of quartz, chlorite, kaolinite, goethite, and, in the lowest part of the profile, siderite. Despite the paucity of quartz in the protolith and 40% removal of SiO2 from the profile, quartz constitutes 11%–23% of the pedogenic mineral assemblage. Like many other Precambrian and Cambrian paleosols in the Lake Superior region, the paleosol experienced potassium metasomatism, now con- taining 10%–25% mixed-layer illite-vermiculite and 5%–44% potassium feldspar. -
Corinna Riginos Curriculum Vitae
Corinna Riginos Curriculum Vitae Berry Biodiversity Conservation Center University of Wyoming Laramie, WY 82071 E-mail: [email protected] Phone (cell): 202-294-9731 Phone (Kenya): +254-20-2033187 EDUCATION PhD 2008 University of California, Davis: Ecology. Dissertation: Tree-grass interactions in an East African savanna: the role of wild and domestic herbivores Graduate advisor: Truman P. Young BS 2000 Brown University: Environmental Science (Magna Cum Laude) POSITIONS 2012- Berry Biodiversity Conservation Postdoctoral Fellow, University of Wyoming 2008-2012 Council on Science and Technology Postdoctoral Fellow and Lecturer, Princeton University 2000-2002 Fulbright U.S. Student Scholar, University of Stellenbosch, South Africa RESEARCH EXPERIENCE 2008-2012 Postdoctoral research: Led design and execution of studies on (a) using livestock to engineer rangelands for wildlife conservation, (b) spatial dynamics of ecosystem functioning, breakdown, and restoration in an African savanna. Additionally, developed methods and manual for pastoralist-based rangeland monitoring under contract from USAID / CARE International. Currently being used on 35,000 km2 in sub-Saharan Africa. Collaborators: Jayne Belnap, Jeff Herrick, Daniel Rubenstein, Kelly Caylor 2003-2005 Doctoral dissertation research: Led design and execution of a series of studies to test causes and consequences of increases in woody vegetation in an African savanna. Statistical modeling and field experimentation. Advisor: Truman Young 2000-2002 Fulbright fellowship: Effects of livestock grazing and disturbance on population and community ecology of succulent shrubs, Succulent Karoo, South Africa. Advisors: Suzanne J. Milton, M. Timm Hoffman 1999-2000 Honors thesis research: Maternal effects of drought stress and inbreeding on a New England forest herb. Advisors: Johanna Schmitt, M. -
Soil Crusts Structural Soil Crusts Are Relatively Thin, Dense, Somewhat Continuous Layers of Non-Aggregated Soil Particles on the Surface of Tilled and Exposed Soils
Indicator Test Function USDA Natural Resources Conservation Service P F W Soil Quality Indicators Soil Crusts Structural soil crusts are relatively thin, dense, somewhat continuous layers of non-aggregated soil particles on the surface of tilled and exposed soils. Structural crusts develop when a sealed-over soil surface dries out after rainfall or irrigation. Water droplets striking soil aggregates and water flowing across soil breaks aggregates into individual soil particles. Fine soil particles wash, settle into and block surface pores causing the soil surface to seal over and preventing water from soaking into the soil. As the muddy soil surface dries out, it crusts over. Left: Note the surface crust on this soil. The field was in tall fescue sod for 11 years. It was cleared and plowed using conventional Structural crusts range from a few tenths to as thick as two tillage methods. Photo courtesy Bobby Brock, USDA NRCS (retired). Right: Collected from a no-till field in Georgia’s Southern inches. A surface crust is much more compact, hard and Piedmont, good structure and aggregation are evident in the soil on brittle when dry than the soil immediately beneath it, the right. The same soil formed a structural crust under which may be loose and friable. Crusts can be described by conventional tillage. Note the sunlight reflectance of the crusted their strength, or air-dry rupture resistance. soil. Photo courtesy James E. Dean, USDA NRCS (retired). Soil crusting is also associated with biological and Dynamic - Management activities that deplete soil chemical factors. A biological crust is a living community organic matter and leave soil bare, smooth and exposed to of lichen, cyanobacteria, algae, and moss growing on the the direct impact of water droplets increase soil dispersion, soil surface that bind the soil together. -
Biological Soil Crust Rehabilitation in Theory and Practice: an Underexploited Opportunity Matthew A
REVIEW Biological Soil Crust Rehabilitation in Theory and Practice: An Underexploited Opportunity Matthew A. Bowker1,2 Abstract techniques; and (3) monitoring. Statistical predictive Biological soil crusts (BSCs) are ubiquitous lichen–bryo- modeling is a useful method for estimating the potential phyte microbial communities, which are critical structural BSC condition of a rehabilitation site. Various rehabilita- and functional components of many ecosystems. How- tion techniques attempt to correct, in decreasing order of ever, BSCs are rarely addressed in the restoration litera- difficulty, active soil erosion (e.g., stabilization techni- ture. The purposes of this review were to examine the ques), resource deficiencies (e.g., moisture and nutrient ecological roles BSCs play in succession models, the augmentation), or BSC propagule scarcity (e.g., inoc- backbone of restoration theory, and to discuss the prac- ulation). Success will probably be contingent on prior tical aspects of rehabilitating BSCs to disturbed eco- evaluation of site conditions and accurate identification systems. Most evidence indicates that BSCs facilitate of constraints to BSC reestablishment. Rehabilitation of succession to later seres, suggesting that assisted recovery BSCs is attainable and may be required in the recovery of of BSCs could speed up succession. Because BSCs are some ecosystems. The strong influence that BSCs exert ecosystem engineers in high abiotic stress systems, loss of on ecosystems is an underexploited opportunity for re- BSCs may be synonymous with crossing degradation storationists to return disturbed ecosystems to a desirable thresholds. However, assisted recovery of BSCs may trajectory. allow a transition from a degraded steady state to a more desired alternative steady state. In practice, BSC rehabili- Key words: aridlands, cryptobiotic soil crusts, cryptogams, tation has three major components: (1) establishment of degradation thresholds, state-and-transition models, goals; (2) selection and implementation of rehabilitation succession. -
The Use of Proximal Soil Sensor Data Fusion and Digital Soil Mapping For
The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, Raphael Viscarra Rossel To cite this version: Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, et al.. The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture. Pedometrics 2017, Jun 2017, Wageningen, Netherlands. 298 p. hal-01601278 HAL Id: hal-01601278 https://hal.archives-ouvertes.fr/hal-01601278 Submitted on 2 Jun 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - ShareAlike| 4.0 International License Abstract Book Pedometrics 2017 Wageningen, 26 June – 1 July 2017 2 Contents Evaluating Use of Ground Penetrating Radar and Geostatistic Methods for Mapping Soil Cemented Horizon .................................... 13 Digital soil mapping in areas of mussunungas: algoritmos comparission .......... 14 Sensing of farm and district-scale soil moisture content using a mobile cosmic ray probe (COSMOS Rover) .................................... 15 Proximal sensing of soil crack networks using three-dimensional electrical resistivity to- mography ......................................... 16 Using digital microscopy for rapid determination of soil texture and prediction of soil organic matter ..................................... -
Native Plant Growth and Seedling Establishment in Soils Influenced by Bromus Tectorum Helen I
Rangeland Ecol Manage 61:630–639 | November 2008 Native Plant Growth and Seedling Establishment in Soils Influenced by Bromus tectorum Helen I. Rowe1 and Cynthia S. Brown2 Authors are 1Research Professor, Forestry and Natural Resources Department, Purdue University, 195 Marsteller Street, West Lafayette, IN 47907, USA; and 2Assistant Professor, Department of Bioagricultural Sciences and Pest Management, 1177 Campus Delivery, Colorado State University, Fort Collins, CO 80523, USA. Abstract The invasion of 40 million hectares of the American West by cheatgrass (Bromus tectorum L.) has caused widespread modifications in the vegetation of semi-arid ecosystems and increased the frequency of fires. In addition to well-understood mechanisms by which cheatgrass gains competitive advantage, it has been implicated in reducing arbuscular mycorrhizal fungi (AMF) abundance and taxa diversity. We evaluated this possibility at a high elevation site in a two-pronged approach. To test whether cheatgrass changed native AMF communities in ways that affected subsequent native plant growth, we grew cheatgrass and native plants in native soils and then planted native plants into these soils in a greenhouse experiment. We found that cheatgrass-influenced soils did not inhibit native plant growth or AMF sporulation or colonization. To test whether soils in cheatgrass-dominated areas inhibited establishment and growth of native plants, cheatgrass was removed and six seeding combinations were applied. We found that 14.02 6 1.7 seedlings ? m22 established and perennial native plant cover increased fourfold over the three years of this study. Glyphosate reduced cheatgrass cover to less than 5% in the year it was applied but did not facilitate native plant establishment or growth compared with no glyphosate. -
Global Environmental and Socio-Economic Impacts of Selected Alien Grasses As a Basis for Ranking Threats to South Africa
A peer-reviewed open-access journal NeoBiota 41: 19–65Global (2018) environmental and socio-economic impacts of selected alien grasses... 19 doi: 10.3897/neobiota.41.26599 RESEARCH ARTICLE NeoBiota http://neobiota.pensoft.net Advancing research on alien species and biological invasions Global environmental and socio-economic impacts of selected alien grasses as a basis for ranking threats to South Africa Khensani V. Nkuna1,2, Vernon Visser3,4, John R.U. Wilson1,2, Sabrina Kumschick1,2 1 South African National Biodiversity Institute, Kirstenbosch Research Centre, Cape Town, South Africa 2 Centre for Invasion Biology, Department of Botany and Zoology, Stellenbosch University, Matieland, 7602, South Africa 3 SEEC – Statistics in Ecology, Environment and Conservation, Department of Statistical Scien- ces, University of Cape Town, Rondebosch, 7701 South Africa 4 African Climate and Development Initiative, University of Cape Town, Rondebosch, 7701, South Africa Corresponding author: Sabrina Kumschick ([email protected]) Academic editor: C. Daehler | Received 14 May 2018 | Accepted 14 November 2018 | Published 21 December 2018 Citation: Nkuna KV, Visser V, Wilson JRU, Kumschick S (2018) Global environmental and socio-economic impacts of selected alien grasses as a basis for ranking threats to South Africa. NeoBiota 41: 19–65. https://doi.org/10.3897/ neobiota.41.26599 Abstract Decisions to allocate management resources should be underpinned by estimates of the impacts of bio- logical invasions that are comparable across species and locations. For the same reason, it is important to assess what type of impacts are likely to occur where, and if such patterns can be generalised. In this paper, we aim to understand factors shaping patterns in the type and magnitude of impacts of a subset of alien grasses. -
National Cooperative Soil Survey and Biological Soil Crusts
Biological Soil Crusts Status Report 2003 National Cooperative Soil Survey Conference Plymouth, Massachusetts June 16 - 20, 2003 Table of Contents I. NCSS 2003 National Conference Proceedings II. Report and recommendations of the soil crust task force - 2002 West Regional Cooperative Soil Survey Conference Task Force Members Charges Part I. Executive Summary and Recommendations Part II. Report on Charges Part III. Research Needs, Action Items, Additional Charges Part IV. Resources for Additional Information Part V. Appendices Appendix 1 - Agency needs Appendix 2 - Draft material for incorporation into the Soil Survey Manual Introduction Relationship to Mineral Crusts Types of Biological Soil Crusts Figure 1. Biological soil crust types. Major Components of Soil Crusts: Cyanobacteria, Lichens, and Mosses Table 1. Morphological groups for biological crust components and their N-fixing characteristics. (Belnap et al. 2001) Soil Surface Roughness/Crust Age Distribution of Crusts References Appendix 3 - Guidelines for describing soil surface features, Version 2.0 Surface features Table 1. Surface features Determining Percent Cover Equipment Method 1. Step-point Method 2. Ocular estimate with quadrats Method 3. Line-point quadrat Method 4. Stratified line-point intercept Method 5. Ocular estimate Appendix 3a - Data sheets used in Moab field test Appendix 4 - Soil descriptions Discussion Group 1 Group 3 Group 2 Group 4 Appendix 5 - Photography Biological Soil Crust Status Report NCSS National Conference June 16-20, 2003 Table of Contents III. Task force's response to the following questions posed by the 2002 West Regional Standards Committee 1. Are biological soil crusts plants, soil or combination of both? 2. Is it appropriate to think of these crusts as plant communities with potentials, state and transition? 3. -
1 Supplementary Information for Invasive Grasses Increase
Supplementary Information For Invasive grasses increase fire occurrence and frequency across U.S. ecoregions Emily J. Fusco1*, John T. Finn2, Jennifer K. Balch3,4, R. Chelsea Nagy3, Bethany A. Bradley1,2 Affiliations: 1 Graduate Program in Organismic and Evolutionary Biology, University of Massachusetts- Amherst, Amherst, Massachusetts, 01003, USA 2 Department of Environmental Conservation, University of Massachusetts- Amherst, Amherst, Massachusetts, 01003, USA 3 Earth Lab, University of Colorado- Boulder, Boulder, Colorado, 80309, USA 4 Department of Geography, University of Colorado-Boulder, Boulder, Colorado, 80309, USA Correspondence to: [email protected] This PDF file includes: Figure S1 Tables S1 to S4 SI References 1 www.pnas.org/cgi/doi/10.1073/pnas.1908253116 Supplemental Table S1: A list of 176 non-native invasive grass and other graminoid species as listed by the Invasive Plant Atlas of the United States (1). For each species, we conducted a Web of Science (WOS) search and recorded whether there was literature suggesting the species altered fire regimes (Yes/No). For each fire promoting species in WOS, we supplemented our determination of whether that species was a fire promoter using the Fire Effects Information System (FEIS; 2). For each species designated as a fire promoter, we searched for available spatial data, and kept only species that were both fire-promoting with spatial data for our analysis. Final species used are highlighted in yellow. WOS FEIS Fire Data Keep for Scientific Name Common Name(s) Search Database Promoter Available Analysis Achnatherum punagrass No - No - No brachychaetum Godr. Barkworth Aegilops cylindrica Host jointed goatgrass No - No - No Aegilops ovate goatgrass No - No - No geniculata Roth Aegilops triuncialis L.