Presentation is loading. Please wait.

Presentation is loading. Please wait.

Lecture 3/4 topics 1.Biomes (what the heck are those?) – Global and local 2.Gradients (physical and biological) 3.How plants grow 4.Productivity and biomass.

Similar presentations

Presentation on theme: "Lecture 3/4 topics 1.Biomes (what the heck are those?) – Global and local 2.Gradients (physical and biological) 3.How plants grow 4.Productivity and biomass."— Presentation transcript:

1 Lecture 3/4 topics 1.Biomes (what the heck are those?) – Global and local 2.Gradients (physical and biological) 3.How plants grow 4.Productivity and biomass – importance in production forestry and carbon sequestration

2 Week 2 Learning Objectives You should be able to: Recognize characteristics and general distribution of biomes and what factors influence their spatial coverage Describe difference between biome based on actual cover and potentialcover (spatially and temporally) Describe various biome/life zone types (globally and locally) and their productivity Understand spatial variation (gradients) in forest types (e.g., elevation, latitude, disturbance, temperature, precipitation) Describe basic photosynthesis and plant productivity (gross primary productivity, net primary productivity, differences in plant requirements) Understand the role of vegetation in carbon storage (sequestration) Think about spatial and temporal differences in ecosystems

3 THE CONCEPT OF BIOMES Biome: a major regional community of plants and animals with similar life forms and environmental conditions. It is the largest geographical biotic unit. How can we tell different biomes apart? Generally named after the dominant type of life form (normally vegetation in terrestrial systems), such as tropical rain forest, grassland, or coral reef.

4 Vegetation serves many critical functions: 1.Produces oxygen via photosynthesis 2. Role in nutrient cycling and energy flows 3. Affects soil characteristics 4. Provides wildlife habitat and energy (food) source 5.Produces food, wood, fuel and other materials for humans 6. Psychologically important to humans, who evolved in direct contact with, and dependence on, vegetation, for food, shelter, and medicine.

5 Much of the work on vegetation classification comes from European and North American ecologists, and they have fundamentally different approaches. North America based on a combination of the following criteria: climate pattern, plant habit, phenology and/or growth form, and dominant species. Europe, classification relies heavily on species composition alone, without explicit reference to climate, phenology or growth forms.

6 Factor for defining biomes Biomes are defined based on factors such as: – plant structures (such as trees, shrubs, and grasses), – leaf types (such as broadleaf and needleleaf), – plant spacing (forest, woodland, savanna), – and other factors like climate, soils, etc. Example systems – Udvardy system -1975 – Bailey system - 1978 – World Wildlife fund – 14 biomes, 852 ecoregions

7 Aquatic Forest Desert Grassland Tundra Five Major Biomes

8 Physical Geography of the Global Environment, 2nd Edition, by H. J. De Blij, et al; 1998 8 major biomes

9 14 major biomes

10 WWF system World Wildlife Fund (WWF) developed an ecological land classification system that identified 14 biomes, called major habitat types, and further divided the world's land area into 825 terrestrial ecoregions. This classification is used to define the list of ecoregions identified by the WWF as priorities for conservation. Tundra(arctic) Boreal forests/taiga (subarctic, humid) Temperate coniferous forests (temperate, humid to semi-humid) Temperate broadleaf and mixed forests (temperate, humid) Temperate grasslands, savannas, and shrublands (temperate, semi-arid) Mediterranean forests, woodlands, and shrub (temperate warm, semi-humid to semi- arid with winter rainfall) Tropical and subtropical coniferous forests (tropical and subtropical, semi-humid) Tropical and subtropical moist broadleaf forests (tropical and subtropical, humid) Tropical and subtropical dry broadleaf forests (tropical and subtropical, semi-humid) Tropical and subtropical grasslands, savannas, and shrublands (tropical and subtropical, and semi-arid) Montane grasslands and shrublands (alpine or montane climate) Deserts and xeric shrublands (temperate to tropical, arid) Mangrove (subtropical and tropical, salt water inundated) Flooded grasslands and savannas (temperate to tropical, fresh or brackish water inundated)

11 In 1975, Miklos Udvardy published a system of 12 terrestrial biomes: Tropical humid forests Subtropical and temperate rainforests or woodlands Temperate broad-leaf forests or woodlands and subpolar deciduous thickets Temperate needle-leaf forests or woodlands Evergreen sclerophyllous forests, scrub, or woodlands Tropical dry or deciduous forests (including Monsoon forests) or woodlands Temperate grasslands Warm deserts and semideserts Cold-winter (continental) deserts and semideserts Tundra communities and barren Arctic deserts Mixed mountain and highland systems with complex zonation Mixed island systems

12 Based on soil moisture and temperature (14 biomes)

13 Kuchler

14 Ponderosa pine Silver firOak Sitka Spruce Grand fir Puget Sound Douglas fir Subalpine fir Western Hemlock Mountain hemlock Interior Douglas fir


16 Humans are major forces in ecosystem structure and function We consume one third of all terrestrial net primary production, We move more earth and produce more reactive nitrogen than all other terrestrial processes combined, We are causing global extinctions and changes in climate that are comparable to any observed in the natural record

17 Rexford F. Daubenmire, 85, professor emeritus of botany at Washington State University, died August 26, 1995 at his home in Mt Plymouth, Florida. He was one of the nation's foremost authorities on plant ecology. Daubenmire's classification of forest and gressland vegetation in the Pacific Northwest became a standard management tool for both government agencies and the timber industry of the West. Considered radical when introduced in the early 1950's, his classification scheme emphasized the potential vegetation of a site, rather than existing vegetation that often had been altered through fire, logging and grazing. He also made lasting contributions in explaining the environmental restrictions that determine the range of tree species, ecological succession, the migration history of plant species in North America, and the role of fire in shaping many plant communities.


19 mora/archaeology/chap2b.htm




23 Biome subdivisions Life Zones (e.g., Merriam 1889, Holdridge 1947) based on observed differences in plant and animal communities that change with physical characteristics – Temperature, latitude, elevations, precipitation, etc. – Ecoregion- (e.g., Bailey 1995, World Wildlife Fund) ecoregions have similar latitudinal and continental locations and are defined by the processes that produce them. The divisions are more specific than biomes, taking into account biogeographical divisions.

24 Holdrige Life Zones Based on biotemperature, precipitation, potential evapotranspiration, and humidity

25 Ecoregions – started by the US Forest Service in 1978, The technique of mapping ecoregions was subsequently expanded to include the rest of North America and the world. In 1993, as part of the Forest Service's National Hierarchical Framework of Ecological Units (ECOMAP).ecoregions were adopted for use in ecosystem management. Robert G. Bailey developed a biogeographical classification system for the United States in a map published in 1975. Bailey subsequently expanded the system to include the rest of North America in 1981, and the world in 1989. The Bailey system is based on climate, and is divided into four domains (Polar, Humid Temperate, Dry, and Humid Tropical), with further divisions based on other climate characteristics (subarctic, warm temperate, hot temperate, and subtropical, marine and continental, lowland and mountain).

26 Bailey



29 b. Physiognomic (or structural – height and spacing of the vegetation) –based on general appearance, dominant life forms, layered structure of plant communities i UNESCO – hierarchical system ii. Current US standard (adopted by the Federal Geographic Data Committee (FGDC), and originally developed by UNESCO and The Nature Conservancy), the classification is hierarchical : system, class, subclass, group, formation, alliance, and association. The lowest level, or association, is thus the most precisely defined, and incorporates the names of the dominant one to three (usually two) species of the type. In practice, the levels of the alliance and/or association are the most often used, particularly in vegetation mapping, just as the Latin binomial is most often used in discussing particular species in taxonomy and in general communication.

30 Nature Conservancy Over the past twenty years, The Nature Conservancy has developed a science-based approach to conserving biological diversity. The Conservancy's approach to conservation science relies on the consistent and systematic accumulation, management, and analysis of information on the "elements of biological diversity" specifically the status and location of plants, animals, and ecological communities. National Vegetation Classification System The national vegetation classification system focuses on existing vegetation rather than potential natural vegetation, climax vegetation, or physical habitats. The vegetation types covered in the classification range from the short-lived to relatively stable and persistent plant communities. The classification includes natural, seminatural, modified, and cultural vegetation. Many regional classification schemes have been developed – For example, in the Pacific Northwest (Daubenmire, Franklin and Dyrness) and British Columbia

31 SAF Forest Cover Type for Western U.S. code name 201White spruce 202 White spruce - paper birch 203 Balsam poplar 204 Black spruce 205 Mountain hemlock 206 Engelmann spruce – subalpine fir 207 Red fir 208 Whitebark pine 209 Bristlecone pine 210 Interior Douglas-fir 211 White fir 212 Western larch 213 Grand fir 215 Western white pine 216 Blue spruce 217 Aspen 218 Lodgepole pine 219 Limber pine 220 Rocky Mountain juniper 221 Red alder 222 Black cottonwood - willow 223 Sitka spruce 224 Western hemlock 225 Western hemlock - Sitka spruce 226 Coastal true fir - hemlock 227 Western redcedar - western hemlock 228 Western redcedar 229 Pacific Douglas-fir 230 Douglas-fir - western hemlock 231 Port Orford-cedar 232 Redwood

32 Example of US standard classification, through association level System: Terrestrial/Aquatic - (hydrological regime) Class: Woodland - (spacing & height of dominant form) Subclass: Evergreen Woodland - (morphological & Phenological similarity) Group: Temperate Evergreen Needle-leaved - (climate latitude, growth form, leaf form) Formation: Evergreen needle-leaved forest with conical crowns - (mapable units) Alliance (or cover type): Abies lasiocarpa Forest (dominant species) Association (or community): Abies lasiocarpa/Vaccinium scoparium [Subalpine fir/Grouseberry] (subdominant or associated species with similar ecological processes)

33 PNV is the "climax" vegetation that will occupy a site without disturbance or climatic change. PNV is an expression of environmental factors such as topography, soils and climate across an area. Where cover type is a classification of existing vegetation, PNV is a site classification based on climax vegetation. Because the existing cover type at any particular location and time may reflect a vegetation community anywhere along its successional pathway - from seral to climax - the cover type may be the same as the PNV. Terrain-matched refinement of Kuchler's Potential Natural Vegetation (PNV) map have been produced. Kuchler's PNV map was digitized for the conterminous United States, then adjusted to match terrain using a 500 m Digital Elevation Model, 4th Code Hydrologic Unit delineations, and Ecological Subregions (Bailey's Sections). These biophysical data layers were integrated with current vegetation layers, Resource Planning Act's Forest Types and Forest Densities of the United States, and USGS EROS Data Center's Land Cover Characterization database, to develop generalized successional pathway diagrams. Expert regional panels refined the PNV map based on these successional pathways.

34 Why classify biomes/vegetation? Better communication among professionals Better understanding of ecosystem interactions Useful aid for land and natural resource management and monitoring, U.S. Forest Service, Forest Inventory Analysis (FIA) plots ( EPA Environmental Monitoring and Assessment Program (EMAP) IUCN Red List for Ecosystems ( Identify the presence of invasive species Ecosystem health issues – climate change, fire effects

35 How can the classifications be used? Corridors Wildlife reintroduction Climate change predictions of distribution Plant restoration

36 Scoring for restoration opportunities

37 Figure 2. Planning unit cost based on naturalness. Schloss CA, Lawler JJ, Larson ER, Papendick HL, et al. (2011) Systematic Conservation Planning in the Face of Climate Change: Bet-Hedging on the Columbia Plateau. PLoS ONE 6(12): e28788. doi:10.1371/journal.pone.0028788 Less natural Columbia Plateau

38 Summary No universal classification scheme Based on various physical, chemical and biological characteristics and assemblages Some based on current vs. potential life forms Some include humans others do not Used for planning, management, restoration

Download ppt "Lecture 3/4 topics 1.Biomes (what the heck are those?) – Global and local 2.Gradients (physical and biological) 3.How plants grow 4.Productivity and biomass."

Similar presentations

Ads by Google