Changes in woody plant cover may be rapid, non-linear, and triggered by extreme environmental events (e.g., drought of 1950s) (from Archer et al. 1988)

Slides:



Advertisements
Similar presentations
Proposed Indicators for Ecological Health & Diversity of Rangelands Rod Heitschmidt, USDA Agricultural Research Service, Miles City, MT and Linda Joyce,
Advertisements

ECOLOGICAL SITES EXPANDING the CONCEPTS and APPLICATIONS of ECOLOGICAL SITES Joel Brown USDA NRCS Jornada Experimental Range Las Cruces NM.
Effects of Land Use Change on Forest Carbon Budgets Throughout the Southern USA from 1900 to 2050 Peter B. Woodbury Crop and Soil Sciences Department,
Nitrogen Mineralization Across an Atmospheric Nitrogen Deposition Gradient in Southern California Deserts Leela E. Rao 1, David R. Parker 1, Andrzej Bytnerowicz.
Carbon storage in silvopastoral systems Farm Woodland Forum Annual Meeting 13 June 2013 Matthew Upson and Paul Burgess Centre for Environmental Risk and.
Vegetation Soil, Landscape Hydrology Process for Assessing Proper Functioning Condition Vegetation Items.
Evergreen tree dynamics in tropical savanna
Tropical Agro-Ecosystems From Rain Forests to Deserts.
Objective: Understand the Concept of Ecological Succession Key Words: Ecological Succession, draining a marsh, clearing woodland to grow crops, strip mining.
Magnitude and Spatial Distribution of Uncertainty in Ecosystem Production and Biomass of Amazonia Caused by Vegetation Characteristics Christopher Potter.
A Day in the Tropical Savanna
Michelle Trogdon GEOG 4401/5401 Soils Geography Fall 2007 – Univ of Colorado, Boulder.
Grassland Biomes Chapter 8.
Konza Prairie Long-Term Ecological Research Station Tall Grass Prairie Ecosystem.
1 Hadley Centre for Climate Prediction and Research Biophysical forcing of climate by anthropogenic vegetation change Richard A. Betts & Pete Falloon Hadley.
Ecosystem services of upland carbon landscapes in England Mick Rebane Evidence Team - Senior Specialist Uplands.
Soils. 3 characteristics of soil affect its value for farming and growing vegetation: 1.Organic Content 2.Mineral Content 3.Soil Texture.
World Forests Forests cover 30% of the world’s land surface.
Arne Grønlund and Daniel P. Rasse Norwegian Institute for Agricultural and Environmental Research Division for Soil and Environment Carbon loss from cultivated.
School Research Conference, March 2009 Jennifer Wright Supervisors: M.Williams, G. Starr, R.Mitchell, M.Mencuccini Fire and Forest Ecosystems in the Southeastern.
Pinyon Juniper Community. Microbiotic Crust Ecological roles for biological crusts 1. Fix carbon and nitrogen 2. Trap dust 3. Increase water retention.
Watersheds and Fire Where conditions are not too dry or too wet and where accumulated carbon from photosynthesis will not oxidize slowly or rot, fire cycles.
CLASS UPDATES Office hours: Fridays 9AM-12noon (or me for an appointment) Powerpoints – on class website Schedule changes: thesis statement, outline,
DESERTS.
Brandy Norville.  A desert is a region with little rain fall.  Less than 10in a year.  Doesn’t have to be sand.  Four major types.  Arid, semi-arid,
Theories of Vegetation Change Mort Kothmann Texas A&M University.
Chapter Soil Chapter 12.4 Soil as a Resource
Effects of Land Cover Change on local and regional climate Ann Thijs Physical Climatology December 1, 2005 Tropical deforestation, Borneo.
Changes to Rangelands Over Time. Range Change Factors  Grazing  Fire  Invasive Species  Weather/Climate  Human Activities.
Australia’s Flora Year 10 Banksia by Sydney Parkinson ( ). Image courtesy of National History Museum, London.
Tropical Grasslands (Savannas)
Biomes: Kinds Of Ecosystem
Lu Liang, Peng Gong Department of Environmental Science, Policy and Management, University of California, Berkeley And Center for Earth System Science,
An important product of Weathering.
Interpreting Ecological Sites for Grazing Management.
Model Intercomparisons and Validation: Terrestrial Carbon, an Arctic Emphasis Andrew Slater.
Long-term vegetation monitoring, an update. Pierre Hiernaux, Eric Mougin, Josiane Seghieri, François Lavenu, Nogmana Soumaguel, Lassine Diarra.
Surface energy (and water) budget in the Sahel during the multi-decadal drought: combining remote sensing and in situ data. Laurent Kergoat (CNRS/LMTG,
How Plants Grow & Respond to Disturbance. Succession & Disturbance  Community change is driven by successional forces: Immigration and establishment.
How Plants Grow & Respond to Disturbance. Succession & Disturbance  Community change is driven by successional forces: Immigration and establishment.
Biomass Production Estimation
Agriculture, Carbon & the climate CO 2 & climate change Moberg et al Source of C emissions Change in temperature & rainfall.
CLIMATE CHANGE EFFECTS ON SOIL CO 2 AND CH 4 FLUXES IN FOUR ECOSYSTEMS ALONG AN ELEVATIONAL GRADIENT IN NORTHERN ARIZONA Joseph C. Blankinship 1, James.
Hydrological and Nutrient Controls on the Structure and Function of Southern African Savannas K.K. Caylor, Paolo D’Odorico, Christelle Hély, Greg Okin,
THE SOIL. Soils are complex mixtures of minerals, water, air, organic matter.
8-3 Savannas   Tropical or subtropical grasslands ranging from scrubland to wet, open woodland. Located in Asia, Africa and South America.
Beneficial Management Practices for Saskatchewan Species at Risk: Sprague’s Pipit Threatened.
Moisture Controls on Trace Gas Fluxes From Semiarid Soils Dean A. Martens and Jean E. T. McLain SWRC – Tucson and Water Conservation Laboratory – Phoenix.
The Effects of Elevated Carbon Dioxide on Microarthropods Jarret M. Childers. Undergraduate at Northern Arizona University. Environmental Science: Management.
Seasonal Emissions of N 2 O, NO, CO and CO 2 in Brazilian Savannas Subjected to Prescribed Fires Alexandre Pinto, Mercedes Bustamante, Laura Viana, Universidade.
George Peacock, Team Leader Grazing Lands Technology Development Team Central National Technology Support Center 2010 Southern Regional Cooperative Soil.
Ecological Sites on Rangeland. A0po&list=PL7CD3CD7A9350A858.
Prediction and modelling of soil erosion…  Why would we want to predict soil erosion? Optimal resource management Evaluation of consequences of different.
Heathland field trip How Polluted!? © Carl Corbidge © Amy Rogers
15 Feet : Minimum Width for Zone 1 Zone 1 Functions: Bank Stabilization Shading (water temperature control) Flood Protection Stream Inputs: Structural.
Ecological Site Descriptions Foundation for Resource Management Decisions George Peacock Grazing Lands Technology Institute USDA-NRCS.
 Natural Vegetation is plant life that hasn’t been planted or changed by humans, it has grown naturally or wildly as nature intended.  Humans however.
Tropical Rainy: Tropical Wet & Dry: Savannas. Tropical Savannas or Grasslands are associated with the tropical wet and dry climate type, but are not generally.
B A C D Native Plant Resiliency Undesired Change A B A C A D B D C D Low severity fire High severity fire/ Overgrazing Repeated high severity fire Desired.
Carbon Dynamics in Coarse Woody Debris Pools at the Tapajos National Forest in Brazil Hudson Silva Patrick Crill Michael Keller.
Response of Understory Vegetation following Western Juniper (Juniperus occidentalis) Cutting on Two Sites Breanna S Sabin FS 533.
Kelsey Perkins. Grasslands are characterized as lands dominated by grasses rather than large shrubs or trees There are two main divisions of grasslands:
Land Biomes 2. Grassland Wet seasons followed by a season of drought 25 to 75 cm precipitation yearly.
Range Values in the Dry Fir Range Practices Specialist
Global Carbon Budget. Global Carbon Budget of the carbon dioxide emitted from anthropogenic sources) -Natural sinks of carbon dioxide are the land.
PRESCRIBED FIRE BASICS
Earth’s Biomes.
Grasslands Grasslands are characterized as lands dominated by grasses rather than large shrubs or trees. There are two main divisions of grasslands: tropical.
Secondary Succession Notes
Rangeland Soil Carbon: State of Knowledge
Presentation transcript:

Changes in woody plant cover may be rapid, non-linear, and triggered by extreme environmental events (e.g., drought of 1950s) (from Archer et al. 1988) Year Woody Cover (%) Site 1 Site 2 Site 3

1950 (3.59 ha) Landscape 1 (1950) Changes in Woody Plant Cover ( ) WoodlandsGrovesClustersHerbaceous La Copita Site, Texas 1976 (5.26 ha) 1990 (6.52 ha)

- 200 yearsPresent+ 200 years (1983) Woody PatchesHerbaceous Patches Area Weighted CO 2 Flux (kg C ha -1 y -1 ) 10%  4%  Annual measurements of soil respiration (McCulley 1999) coupled with a successional model of vegetation change (Scanlan & Archer 1991), indicate successional model of vegetation change (Scanlan & Archer 1991), indicate soil CO 2 flux may have increased ca. 10% subsequent to woody plant soil CO 2 flux may have increased ca. 10% subsequent to woody plantencroachment

(from Hibbard et al. 2000) Annual N min in southern Texas are highest in soils associated with woody vegetation known to have developed over the past century AnnualN-Mineralization Patch Type(µg g -1 y -1 ) Herbaceous Shrub Cluster Grove Woodland

NITRIC OXIDE FLUXES La Copita Site, Texas (from Cole et al. 1996) mg NO cm -2 hr -1 Wet Soil Dry Soil Herbaceous Patch Grove Patch Woodland Patch Upland, Sandy Loam Low land, Clay Loam

Increases in woody plant abundance have increased NMHC emissions 3-fold at the La Copita site.

Soil Organic Carbon (kg m -2 ) SOC in Grazed Grasslands La Copita Site, Texas (from Hibbard 1995) Year Onset of Heavy Grazing Lowland (Clay Loam) Upland (Sandy Loam)

Year Plant Carbon (kg m -2 ) Historical Changes in Plant Carbon Pool La Copita Site, Texas (from Hibbard 1995) La Copita Site, Texas (from Hibbard 1995) Grass + Woody Patches "Pristine" Grassland Heavily Grazed Grassland

Year Grass + Woody Patches "Pristine" Grassland Heavily Grazed Grassland Soil Organic Carbon (kg m -2 ) Historical Changes in Soil Carbon Pool La Copita Site, Texas (from Hibbard 1995)

Estimates of C-sequestration by dryland woody plants must account for deep root systems plants must account for deep root systems (photo by S. Archer, La Copita site, Texas) (photo by S. Archer, La Copita site, Texas)

high Woody plant establishment Tree-shrub community development heavy, continuous grazing heavy, continuous grazing elimination of fire elimination of fire minimal browsing minimal browsing Time Time low Nutrient pools & fluxes ProductivityBiodiversity (from Archer et al. 2000) Degradation Phase Degradation Phase Tree/shrub-driven Tree/shrub-driven succession succession Aggradation Phase Aggradation Phase Herbaceousretrogression