SlideShare ist ein Scribd-Unternehmen logo
1 von 69
CHAPTERS 21-23
PRESENTED BY: LEANDRO MICHAEL C. DE LOS SANTOS, JR.
CHAPTER 21
Ecosystem Energetics
1. Describe the effects of temperature,
moisture, length of photosynthetic period,
and nutrient availability on net primary
productivity in terrestrial ecosystems.
Terms to define:
Net Primary Productivity (NPP)- is the rate of
energy storage as organic matter after respiration
Gross Primary Productivity (GPP)- total rate of
photosynthesis or energy assimilated by the
autothrophs
Factors limiting primary productivity in terrestrial
ecosystems
 Temperature
 Precipitation
 Light
 Nutrients
Global map of primary productivity
To summarize:
Temperature + Precipitation = NPP
Temperature + Precipitation = NPP
Temperature + Precipitation = NPP
Temperature = Length of Photosynthesis = NPP
Nutrients = Nutrient uptake,
photosynthesis & plant growth =
NPP
2. Explain why primary
productivity is typically higher in
coastal areas of the ocean than far
from shore in the open ocean.
3. Explain the difference between
primary production and secondary
production. How is secondary
production affected by primary
production?
Primary Production- production by
green plants over time
Secondary Production- production by
consumer organisms over time which
include consumption of energy from
the produces which is then used for
metabolic activities
Primary productivity
limits secondary
productivity
4. What are the two main food chains
of ecosystems? Which is more
dominant in terrestrial ecosystems and
why?
Grazing food chain- the source of energy is living
plant biomass or net primary production
ex. Cattle grazing on pastureland, insect feeding
on leaves, zooplankton feeding on phytoplankton
Detrital food chain- source of energy is dead
organic matter or detritus
ex. snails, bettles, millipeds, earthworms, fungi &
bacteria
2 Food chains
Detrital food chain is the most common food
chain in all ecosystems since most ungrazed or
unconsumed energy is returned to the soil as
dead material.
In a yellow poplar forest
maintenance & respiration 50%
new tissue 13%
consumed by herbivores 2%
Detrital food chain 35%
5. Explain why energy is lost as it is
transferred from one trophic level to
another. What are the effects of energy
loss on the biomass of different trophic
levels?
Trophic efficiency- ratio of productivity in a given
trophic level to the trophic level it feeds on
6. How do humans affect net primary
productivity? Does the affluence of a
society affect how humans appropriate
net primary productivity?
• Human species consume a vast amount of
Earth’s resources
• In a study conducted by Vitousek, et. al they
used 3 approaches to estimate human NPP
appropriation:
 low estimate- food, fuel, fiber, timber
 intermediate estimate- productivity of
lands devoted to human activities
 high estimate- conversion of lands to
cities, forests to pastures or overgrazing
or excessive erosion
Both population and per capita consumption
interact to determine the human ecological
impact on regional scale.
Affluence also affect net primary productivity
among humans. Developed countries have
double HANPP compared to developing nations
CHAPTER 22
Decomposition and Nutrient Cycling
1. Describe the movement of an atom of
nitrogen from the leaf of a plant,
through the process of decomposition,
and back into the root of another plant.
2. Describe three different processes
that are important for decomposition.
Explain which organisms are important
for each of the processes.
Decomposition processes:
1. Leaching- dissolving and washing of
nutrients out of soil, litter and organic matter
ex. bacteria and fungi
2. Fragmentation- disintegration of organic
matter by invertebrate detritivores such as
protozoans, nematodes, millipedes, etc.
3. Ingestion & excretion of waste products-
heterotrophs function as decomposers by
digesting food, break down organic matter,
3. Discuss the effects of temperature,
humidity, and oxygen availability on
the rate of decomposition.
2 things related to decomposition rate:
 the quality of plant litter as a substrate for
microorganisms and soil fauna active in the
decomposition process
 Features of the physical environment that
directly influence decomposer populations
like soil properties and climate
4. Explain how the "quality" of plant-
derived organic matter changes during
the course of decomposition.
5. Define mineralization and immobilization,
and discuss the differences between them
Mineralization- microbial breakdown of humus and
other organic matter in soil to inorganic matter esp
into its ionic form such as ammonium, sulfate and
phosphate
Immobilization- conversion of an element from
inorganic to organic form in microbial or plant tissue,
rendering the nutrient unavailable to other organisms
6. Describe two major differences between
decomposition in terrestrial environments
and
decomposition in aquatic environments.
Terrestrial Decomposition
 decomposition is a soil process
 involves two size-based animal groups; the
macrofauna and the microfauna
 primary production and decomposition is linked
by vegetation
(Source: http://ww2.tnstate.edu)
Aquatic Decomposition
 macrofauna found in freshwater is similar to
those found in soils except for millipedes, in
marine, there are no insects instead there are
polychaetes and many crustaceans
 in aquatic systems, the photic zone may be
separated from the benthos (where most
decomposition goes on)
 nutrients are only mixed into the photic zone
when thermocline breaks down and Turnover
of the body of water can occur
(Source: http://ww2.tnstate.edu)
7. Describe one major difference between
nutrient cycling in a river and nutrient
cycling in a lake
Nutrient Cycling in Lakes
Nutrient Cycling in Rivers (Nutrient Spiraling)
8. Describe the process of upwelling in
the ocean and how it relates to fisheries
What is upwelling?
Winds blowing across the
ocean surface push water
away. Water then rises up
from beneath the surface to
replace the water that was
pushed away
Source: www.oceanservice.noaa.gov
Water that rises to the surface as a result of
upwelling is rich in nutrients. These nutrients
“fertilize” surface waters and therefore are good
fishing grounds due too high biological
productivity
9. Describe how you might go about
measuring the rate of decomposition of leaf
litter in the upper layer of a forest soil.
CHAPTER 23
Biogeochemical Cycles
1. Explain the difference between the
two basic types of biogeochemical
cycles, using specific examples of each.
What is biogeochemical cycle?
•any of the natural circulation pathways of the
essential elements of living matter. These elements
in various forms flow from the nonliving (abiotic)
to the living (biotic) components of the biosphere
and back to the nonliving again
2 Major types of biogeochemical cycles:
1. gaseous- main pool of nutrients are the
atmosphere and oceans (via evaporation)ex.
carbon, nitrogen, oxgen, carbon and water
2. sedimentary- main pool of nutrients are the
rocks, soil and minerals (Earth’s crust) ex. iron,
phosphorous, sulfur & other earthbound
elements
2. Describe three ways that nutrients
can be lost from an ecosystem
3 ways of nutrient loss in the ecosystem:
1. Export of nutrients
 carbon being exported to the atmosphere via
respiration
 microbial and plant processes being transformed
to nutrients in a gaseous phase
 Organic matter being carried from the ecosystem
through surface flow of water in streams & rivers
3 ways of nutrient loss in the ecosystem:
2. Harvesting
 Biomass harvest such as in farming and logging
3. Fire
 Kills vegetation and converts some biomass to soil
organic matter to ash
 If not taken up by vegetation during recovery,
nutrients may be lost through leaching and
erosion
3. Describe how atmospheric carbon dioxide
levels fluctuate daily, seasonally, and
geographically. Explain why such fluctuation
occurs.
Atmospheric carbon dioxide levels fluctuate on a
daily basis due to:
 consistency
 photosynthetic stages during the day
 less carbon dioxide gathered during sunlight
gathering
Atmospheric carbon dioxide levels fluctuate
seasonally and geographically due to:
 temperature
 solar radiation
 timing of the growing and dormant seasons
 land area
4. Describe a pathway of nitrogen from the
atmosphere into the body tissue of an
herbivore.
Nitrogen cycle: Fixation
Biological
Fixation
Mineralization
Assimilation
Consumption by
herbivores
5. Describe how an atom of phosphorus
might move from the crystal lattice of a
mineral in a rock, through a plant, and into
the ocean.
 phosphate salts are release from rocks
through weathering, leaching, erosion,
mining or agricultural fertilizers usually
dissolved in water
 dissolved phosphate being absorbed by
plants
 animals absorb phosphates by eating plants
or plant-eating animals
 when animals or plants die, phosphates
returns to the soil or ocean
(source: http://www.lenntech.com)
6. List and describe three different inputs of
sulfur into the atmosphere.
Sulfur enters the atmosphere from several sources:
1. combustion of fossil fuels
2. volcanic eruptions
3. exchange at the surface of the oceans
7. Describe how ozone is formed at different
levels of the atmosphere and how biological
organisms are affected by ozone.
Source: http://www.ozonelayer.noaa.gov
Chapters 21 23 ecology

Weitere ähnliche Inhalte

Was ist angesagt?

Was ist angesagt? (20)

Biological communities
Biological communitiesBiological communities
Biological communities
 
5.1 communities & ecosystems
5.1 communities & ecosystems5.1 communities & ecosystems
5.1 communities & ecosystems
 
Topic 3.2
Topic 3.2Topic 3.2
Topic 3.2
 
Community Ecology
Community EcologyCommunity Ecology
Community Ecology
 
Mutualism, Species Abundance, and Diversity
Mutualism, Species Abundance, and DiversityMutualism, Species Abundance, and Diversity
Mutualism, Species Abundance, and Diversity
 
Ch. 42 PowerPoint POL2e
Ch. 42 PowerPoint POL2eCh. 42 PowerPoint POL2e
Ch. 42 PowerPoint POL2e
 
ecological extinction
  ecological extinction  ecological extinction
ecological extinction
 
Biodiversity Basics
Biodiversity BasicsBiodiversity Basics
Biodiversity Basics
 
The Theory of Evolution and its limits
The Theory of Evolution and its limitsThe Theory of Evolution and its limits
The Theory of Evolution and its limits
 
Limiting factors
Limiting factorsLimiting factors
Limiting factors
 
Ecotone and edge effects & ecological succession
Ecotone and edge effects & ecological successionEcotone and edge effects & ecological succession
Ecotone and edge effects & ecological succession
 
Community ecology
Community ecology Community ecology
Community ecology
 
Community ecology
Community ecologyCommunity ecology
Community ecology
 
Biodiversity
BiodiversityBiodiversity
Biodiversity
 
1. environmental ethics
1. environmental ethics1. environmental ethics
1. environmental ethics
 
17.1 The History of Classification
17.1 The History of Classification17.1 The History of Classification
17.1 The History of Classification
 
Pre IB Biology Ecology
Pre IB Biology Ecology Pre IB Biology Ecology
Pre IB Biology Ecology
 
38 Lecture Ppt
38 Lecture Ppt38 Lecture Ppt
38 Lecture Ppt
 
Ecology & Ecosystems
Ecology & EcosystemsEcology & Ecosystems
Ecology & Ecosystems
 
Environmental studies
Environmental studiesEnvironmental studies
Environmental studies
 

Andere mochten auch (13)

Atmosphere
AtmosphereAtmosphere
Atmosphere
 
Continental solids
Continental solidsContinental solids
Continental solids
 
Chapters 17 20 ecology
Chapters 17 20 ecologyChapters 17 20 ecology
Chapters 17 20 ecology
 
Chapters 8 11 ecology
Chapters 8 11 ecologyChapters 8 11 ecology
Chapters 8 11 ecology
 
Construction & demolition waste
Construction & demolition wasteConstruction & demolition waste
Construction & demolition waste
 
Applications of biotechnology in cancer
Applications of biotechnology in cancerApplications of biotechnology in cancer
Applications of biotechnology in cancer
 
Chapter 6 7 ecology
Chapter 6 7 ecologyChapter 6 7 ecology
Chapter 6 7 ecology
 
Inorganic nutrients
Inorganic nutrientsInorganic nutrients
Inorganic nutrients
 
Chapter 21- Populations and Communities
Chapter 21- Populations and CommunitiesChapter 21- Populations and Communities
Chapter 21- Populations and Communities
 
Topic 2 -The Ecosystem Powerpoint
Topic 2 -The Ecosystem PowerpointTopic 2 -The Ecosystem Powerpoint
Topic 2 -The Ecosystem Powerpoint
 
Dissolved oxygen
Dissolved oxygenDissolved oxygen
Dissolved oxygen
 
Chapter 21 Ecology Lesson 1 - Biotic and abiotic factors
Chapter 21 Ecology Lesson 1 - Biotic and abiotic factorsChapter 21 Ecology Lesson 1 - Biotic and abiotic factors
Chapter 21 Ecology Lesson 1 - Biotic and abiotic factors
 
Ecology notes ppt
Ecology notes pptEcology notes ppt
Ecology notes ppt
 

Ähnlich wie Chapters 21 23 ecology

Ecosystem and The Flow of Energy in an Ecosytem
Ecosystem and The Flow of Energy in an EcosytemEcosystem and The Flow of Energy in an Ecosytem
Ecosystem and The Flow of Energy in an EcosytemAmos Watentena
 
Pertemuan 01 produktivity
Pertemuan 01 produktivityPertemuan 01 produktivity
Pertemuan 01 produktivityEko Efendi
 
Organisms and Environment - Part I
Organisms and Environment - Part IOrganisms and Environment - Part I
Organisms and Environment - Part IEdnexa
 
Environmental Segments and Natural/Biogeochemical cycles
Environmental Segments and Natural/Biogeochemical cyclesEnvironmental Segments and Natural/Biogeochemical cycles
Environmental Segments and Natural/Biogeochemical cyclesPRANSHU KUMAR GUPTA
 
Ecologyandecosystem 141103053114-conversion-gate02
Ecologyandecosystem 141103053114-conversion-gate02Ecologyandecosystem 141103053114-conversion-gate02
Ecologyandecosystem 141103053114-conversion-gate02Sandhya Thakkar
 
Bioocean1 :Introduction to Biological Oceanography
Bioocean1 :Introduction to Biological Oceanography Bioocean1 :Introduction to Biological Oceanography
Bioocean1 :Introduction to Biological Oceanography Gazi Abdullah
 
Primary and secondary production, landscape ecology and ecological modeling.
Primary and secondary production, landscape ecology and ecological modeling.Primary and secondary production, landscape ecology and ecological modeling.
Primary and secondary production, landscape ecology and ecological modeling.Ateeqa Ijaz
 
EnvironmentalChemistry lecture 1 (422).pdf
EnvironmentalChemistry lecture 1 (422).pdfEnvironmentalChemistry lecture 1 (422).pdf
EnvironmentalChemistry lecture 1 (422).pdfMaiMostafa61
 
12 biology notes_ch14_ecosystem
12 biology notes_ch14_ecosystem12 biology notes_ch14_ecosystem
12 biology notes_ch14_ecosystemMayank Sharma
 
Environment Education/Earth Education.pptx
Environment Education/Earth Education.pptxEnvironment Education/Earth Education.pptx
Environment Education/Earth Education.pptxgenopaolog
 
6706524360692465dfdvdcdsfgrbhb s213.ppt
6706524360692465dfdvdcdsfgrbhb  s213.ppt6706524360692465dfdvdcdsfgrbhb  s213.ppt
6706524360692465dfdvdcdsfgrbhb s213.pptGeraldineMinong1
 
Ecology 2: Energy & Biodiversity NOTES
Ecology 2: Energy & Biodiversity NOTESEcology 2: Energy & Biodiversity NOTES
Ecology 2: Energy & Biodiversity NOTESRobin Seamon
 

Ähnlich wie Chapters 21 23 ecology (20)

Ecosystem and The Flow of Energy in an Ecosytem
Ecosystem and The Flow of Energy in an EcosytemEcosystem and The Flow of Energy in an Ecosytem
Ecosystem and The Flow of Energy in an Ecosytem
 
Pertemuan 01 produktivity
Pertemuan 01 produktivityPertemuan 01 produktivity
Pertemuan 01 produktivity
 
Organisms and Environment - Part I
Organisms and Environment - Part IOrganisms and Environment - Part I
Organisms and Environment - Part I
 
Environmental Segments and Natural/Biogeochemical cycles
Environmental Segments and Natural/Biogeochemical cyclesEnvironmental Segments and Natural/Biogeochemical cycles
Environmental Segments and Natural/Biogeochemical cycles
 
Concept of ecosystem
Concept of ecosystemConcept of ecosystem
Concept of ecosystem
 
Multidisciplinary Nature Of Environmental studies
Multidisciplinary Nature Of Environmental studies Multidisciplinary Nature Of Environmental studies
Multidisciplinary Nature Of Environmental studies
 
Ecologyandecosystem 141103053114-conversion-gate02
Ecologyandecosystem 141103053114-conversion-gate02Ecologyandecosystem 141103053114-conversion-gate02
Ecologyandecosystem 141103053114-conversion-gate02
 
Chapter ten
Chapter tenChapter ten
Chapter ten
 
Biogeochemical cycles
Biogeochemical cyclesBiogeochemical cycles
Biogeochemical cycles
 
Bioocean1 :Introduction to Biological Oceanography
Bioocean1 :Introduction to Biological Oceanography Bioocean1 :Introduction to Biological Oceanography
Bioocean1 :Introduction to Biological Oceanography
 
Primary and secondary production, landscape ecology and ecological modeling.
Primary and secondary production, landscape ecology and ecological modeling.Primary and secondary production, landscape ecology and ecological modeling.
Primary and secondary production, landscape ecology and ecological modeling.
 
EnvironmentalChemistry lecture 1 (422).pdf
EnvironmentalChemistry lecture 1 (422).pdfEnvironmentalChemistry lecture 1 (422).pdf
EnvironmentalChemistry lecture 1 (422).pdf
 
12 biology notes_ch14_ecosystem
12 biology notes_ch14_ecosystem12 biology notes_ch14_ecosystem
12 biology notes_ch14_ecosystem
 
Environment Education/Earth Education.pptx
Environment Education/Earth Education.pptxEnvironment Education/Earth Education.pptx
Environment Education/Earth Education.pptx
 
Ecosystem
EcosystemEcosystem
Ecosystem
 
6706524360692465dfdvdcdsfgrbhb s213.ppt
6706524360692465dfdvdcdsfgrbhb  s213.ppt6706524360692465dfdvdcdsfgrbhb  s213.ppt
6706524360692465dfdvdcdsfgrbhb s213.ppt
 
Biodiversity
BiodiversityBiodiversity
Biodiversity
 
Ecology 2: Energy & Biodiversity NOTES
Ecology 2: Energy & Biodiversity NOTESEcology 2: Energy & Biodiversity NOTES
Ecology 2: Energy & Biodiversity NOTES
 
7Eutrophication.pdf
7Eutrophication.pdf7Eutrophication.pdf
7Eutrophication.pdf
 
2019 tg biosphere
2019 tg biosphere2019 tg biosphere
2019 tg biosphere
 

Kürzlich hochgeladen

Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptxUnlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptxanandsmhk
 
Formation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksFormation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksSérgio Sacani
 
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...ssifa0344
 
Green chemistry and Sustainable development.pptx
Green chemistry  and Sustainable development.pptxGreen chemistry  and Sustainable development.pptx
Green chemistry and Sustainable development.pptxRajatChauhan518211
 
Disentangling the origin of chemical differences using GHOST
Disentangling the origin of chemical differences using GHOSTDisentangling the origin of chemical differences using GHOST
Disentangling the origin of chemical differences using GHOSTSérgio Sacani
 
Bentham & Hooker's Classification. along with the merits and demerits of the ...
Bentham & Hooker's Classification. along with the merits and demerits of the ...Bentham & Hooker's Classification. along with the merits and demerits of the ...
Bentham & Hooker's Classification. along with the merits and demerits of the ...Nistarini College, Purulia (W.B) India
 
Zoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfZoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfSumit Kumar yadav
 
Biological Classification BioHack (3).pdf
Biological Classification BioHack (3).pdfBiological Classification BioHack (3).pdf
Biological Classification BioHack (3).pdfmuntazimhurra
 
Spermiogenesis or Spermateleosis or metamorphosis of spermatid
Spermiogenesis or Spermateleosis or metamorphosis of spermatidSpermiogenesis or Spermateleosis or metamorphosis of spermatid
Spermiogenesis or Spermateleosis or metamorphosis of spermatidSarthak Sekhar Mondal
 
A relative description on Sonoporation.pdf
A relative description on Sonoporation.pdfA relative description on Sonoporation.pdf
A relative description on Sonoporation.pdfnehabiju2046
 
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRStunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRDelhi Call girls
 
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43bNightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43bSérgio Sacani
 
Botany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfBotany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfSumit Kumar yadav
 
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptx
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptxSOLUBLE PATTERN RECOGNITION RECEPTORS.pptx
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptxkessiyaTpeter
 
Orientation, design and principles of polyhouse
Orientation, design and principles of polyhouseOrientation, design and principles of polyhouse
Orientation, design and principles of polyhousejana861314
 
Animal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxAnimal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxUmerFayaz5
 
Presentation Vikram Lander by Vedansh Gupta.pptx
Presentation Vikram Lander by Vedansh Gupta.pptxPresentation Vikram Lander by Vedansh Gupta.pptx
Presentation Vikram Lander by Vedansh Gupta.pptxgindu3009
 
Botany 4th semester series (krishna).pdf
Botany 4th semester series (krishna).pdfBotany 4th semester series (krishna).pdf
Botany 4th semester series (krishna).pdfSumit Kumar yadav
 

Kürzlich hochgeladen (20)

Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptxUnlocking  the Potential: Deep dive into ocean of Ceramic Magnets.pptx
Unlocking the Potential: Deep dive into ocean of Ceramic Magnets.pptx
 
Engler and Prantl system of classification in plant taxonomy
Engler and Prantl system of classification in plant taxonomyEngler and Prantl system of classification in plant taxonomy
Engler and Prantl system of classification in plant taxonomy
 
Formation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disksFormation of low mass protostars and their circumstellar disks
Formation of low mass protostars and their circumstellar disks
 
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...
TEST BANK For Radiologic Science for Technologists, 12th Edition by Stewart C...
 
Green chemistry and Sustainable development.pptx
Green chemistry  and Sustainable development.pptxGreen chemistry  and Sustainable development.pptx
Green chemistry and Sustainable development.pptx
 
The Philosophy of Science
The Philosophy of ScienceThe Philosophy of Science
The Philosophy of Science
 
Disentangling the origin of chemical differences using GHOST
Disentangling the origin of chemical differences using GHOSTDisentangling the origin of chemical differences using GHOST
Disentangling the origin of chemical differences using GHOST
 
Bentham & Hooker's Classification. along with the merits and demerits of the ...
Bentham & Hooker's Classification. along with the merits and demerits of the ...Bentham & Hooker's Classification. along with the merits and demerits of the ...
Bentham & Hooker's Classification. along with the merits and demerits of the ...
 
Zoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdfZoology 4th semester series (krishna).pdf
Zoology 4th semester series (krishna).pdf
 
Biological Classification BioHack (3).pdf
Biological Classification BioHack (3).pdfBiological Classification BioHack (3).pdf
Biological Classification BioHack (3).pdf
 
Spermiogenesis or Spermateleosis or metamorphosis of spermatid
Spermiogenesis or Spermateleosis or metamorphosis of spermatidSpermiogenesis or Spermateleosis or metamorphosis of spermatid
Spermiogenesis or Spermateleosis or metamorphosis of spermatid
 
A relative description on Sonoporation.pdf
A relative description on Sonoporation.pdfA relative description on Sonoporation.pdf
A relative description on Sonoporation.pdf
 
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCRStunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
Stunning ➥8448380779▻ Call Girls In Panchshil Enclave Delhi NCR
 
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43bNightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
Nightside clouds and disequilibrium chemistry on the hot Jupiter WASP-43b
 
Botany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdfBotany 4th semester file By Sumit Kumar yadav.pdf
Botany 4th semester file By Sumit Kumar yadav.pdf
 
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptx
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptxSOLUBLE PATTERN RECOGNITION RECEPTORS.pptx
SOLUBLE PATTERN RECOGNITION RECEPTORS.pptx
 
Orientation, design and principles of polyhouse
Orientation, design and principles of polyhouseOrientation, design and principles of polyhouse
Orientation, design and principles of polyhouse
 
Animal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptxAnimal Communication- Auditory and Visual.pptx
Animal Communication- Auditory and Visual.pptx
 
Presentation Vikram Lander by Vedansh Gupta.pptx
Presentation Vikram Lander by Vedansh Gupta.pptxPresentation Vikram Lander by Vedansh Gupta.pptx
Presentation Vikram Lander by Vedansh Gupta.pptx
 
Botany 4th semester series (krishna).pdf
Botany 4th semester series (krishna).pdfBotany 4th semester series (krishna).pdf
Botany 4th semester series (krishna).pdf
 

Chapters 21 23 ecology

  • 1. CHAPTERS 21-23 PRESENTED BY: LEANDRO MICHAEL C. DE LOS SANTOS, JR.
  • 3. 1. Describe the effects of temperature, moisture, length of photosynthetic period, and nutrient availability on net primary productivity in terrestrial ecosystems.
  • 4. Terms to define: Net Primary Productivity (NPP)- is the rate of energy storage as organic matter after respiration Gross Primary Productivity (GPP)- total rate of photosynthesis or energy assimilated by the autothrophs
  • 5. Factors limiting primary productivity in terrestrial ecosystems  Temperature  Precipitation  Light  Nutrients
  • 6.
  • 7.
  • 8. Global map of primary productivity
  • 9. To summarize: Temperature + Precipitation = NPP Temperature + Precipitation = NPP Temperature + Precipitation = NPP Temperature = Length of Photosynthesis = NPP Nutrients = Nutrient uptake, photosynthesis & plant growth = NPP
  • 10. 2. Explain why primary productivity is typically higher in coastal areas of the ocean than far from shore in the open ocean.
  • 11.
  • 12. 3. Explain the difference between primary production and secondary production. How is secondary production affected by primary production?
  • 13. Primary Production- production by green plants over time Secondary Production- production by consumer organisms over time which include consumption of energy from the produces which is then used for metabolic activities
  • 15. 4. What are the two main food chains of ecosystems? Which is more dominant in terrestrial ecosystems and why?
  • 16. Grazing food chain- the source of energy is living plant biomass or net primary production ex. Cattle grazing on pastureland, insect feeding on leaves, zooplankton feeding on phytoplankton Detrital food chain- source of energy is dead organic matter or detritus ex. snails, bettles, millipeds, earthworms, fungi & bacteria
  • 18. Detrital food chain is the most common food chain in all ecosystems since most ungrazed or unconsumed energy is returned to the soil as dead material. In a yellow poplar forest maintenance & respiration 50% new tissue 13% consumed by herbivores 2% Detrital food chain 35%
  • 19. 5. Explain why energy is lost as it is transferred from one trophic level to another. What are the effects of energy loss on the biomass of different trophic levels?
  • 20. Trophic efficiency- ratio of productivity in a given trophic level to the trophic level it feeds on
  • 21.
  • 22. 6. How do humans affect net primary productivity? Does the affluence of a society affect how humans appropriate net primary productivity?
  • 23. • Human species consume a vast amount of Earth’s resources • In a study conducted by Vitousek, et. al they used 3 approaches to estimate human NPP appropriation:  low estimate- food, fuel, fiber, timber  intermediate estimate- productivity of lands devoted to human activities  high estimate- conversion of lands to cities, forests to pastures or overgrazing or excessive erosion
  • 24. Both population and per capita consumption interact to determine the human ecological impact on regional scale. Affluence also affect net primary productivity among humans. Developed countries have double HANPP compared to developing nations
  • 25. CHAPTER 22 Decomposition and Nutrient Cycling
  • 26. 1. Describe the movement of an atom of nitrogen from the leaf of a plant, through the process of decomposition, and back into the root of another plant.
  • 27.
  • 28.
  • 29. 2. Describe three different processes that are important for decomposition. Explain which organisms are important for each of the processes.
  • 30. Decomposition processes: 1. Leaching- dissolving and washing of nutrients out of soil, litter and organic matter ex. bacteria and fungi 2. Fragmentation- disintegration of organic matter by invertebrate detritivores such as protozoans, nematodes, millipedes, etc. 3. Ingestion & excretion of waste products- heterotrophs function as decomposers by digesting food, break down organic matter,
  • 31. 3. Discuss the effects of temperature, humidity, and oxygen availability on the rate of decomposition.
  • 32. 2 things related to decomposition rate:  the quality of plant litter as a substrate for microorganisms and soil fauna active in the decomposition process  Features of the physical environment that directly influence decomposer populations like soil properties and climate
  • 33.
  • 34.
  • 35. 4. Explain how the "quality" of plant- derived organic matter changes during the course of decomposition.
  • 36.
  • 37. 5. Define mineralization and immobilization, and discuss the differences between them
  • 38. Mineralization- microbial breakdown of humus and other organic matter in soil to inorganic matter esp into its ionic form such as ammonium, sulfate and phosphate Immobilization- conversion of an element from inorganic to organic form in microbial or plant tissue, rendering the nutrient unavailable to other organisms
  • 39.
  • 40. 6. Describe two major differences between decomposition in terrestrial environments and decomposition in aquatic environments.
  • 41. Terrestrial Decomposition  decomposition is a soil process  involves two size-based animal groups; the macrofauna and the microfauna  primary production and decomposition is linked by vegetation (Source: http://ww2.tnstate.edu)
  • 42. Aquatic Decomposition  macrofauna found in freshwater is similar to those found in soils except for millipedes, in marine, there are no insects instead there are polychaetes and many crustaceans  in aquatic systems, the photic zone may be separated from the benthos (where most decomposition goes on)  nutrients are only mixed into the photic zone when thermocline breaks down and Turnover of the body of water can occur (Source: http://ww2.tnstate.edu)
  • 43.
  • 44. 7. Describe one major difference between nutrient cycling in a river and nutrient cycling in a lake
  • 46. Nutrient Cycling in Rivers (Nutrient Spiraling)
  • 47. 8. Describe the process of upwelling in the ocean and how it relates to fisheries
  • 48. What is upwelling? Winds blowing across the ocean surface push water away. Water then rises up from beneath the surface to replace the water that was pushed away Source: www.oceanservice.noaa.gov
  • 49. Water that rises to the surface as a result of upwelling is rich in nutrients. These nutrients “fertilize” surface waters and therefore are good fishing grounds due too high biological productivity
  • 50. 9. Describe how you might go about measuring the rate of decomposition of leaf litter in the upper layer of a forest soil.
  • 52. 1. Explain the difference between the two basic types of biogeochemical cycles, using specific examples of each.
  • 53. What is biogeochemical cycle? •any of the natural circulation pathways of the essential elements of living matter. These elements in various forms flow from the nonliving (abiotic) to the living (biotic) components of the biosphere and back to the nonliving again
  • 54. 2 Major types of biogeochemical cycles: 1. gaseous- main pool of nutrients are the atmosphere and oceans (via evaporation)ex. carbon, nitrogen, oxgen, carbon and water 2. sedimentary- main pool of nutrients are the rocks, soil and minerals (Earth’s crust) ex. iron, phosphorous, sulfur & other earthbound elements
  • 55. 2. Describe three ways that nutrients can be lost from an ecosystem
  • 56. 3 ways of nutrient loss in the ecosystem: 1. Export of nutrients  carbon being exported to the atmosphere via respiration  microbial and plant processes being transformed to nutrients in a gaseous phase  Organic matter being carried from the ecosystem through surface flow of water in streams & rivers
  • 57. 3 ways of nutrient loss in the ecosystem: 2. Harvesting  Biomass harvest such as in farming and logging 3. Fire  Kills vegetation and converts some biomass to soil organic matter to ash  If not taken up by vegetation during recovery, nutrients may be lost through leaching and erosion
  • 58. 3. Describe how atmospheric carbon dioxide levels fluctuate daily, seasonally, and geographically. Explain why such fluctuation occurs.
  • 59. Atmospheric carbon dioxide levels fluctuate on a daily basis due to:  consistency  photosynthetic stages during the day  less carbon dioxide gathered during sunlight gathering
  • 60. Atmospheric carbon dioxide levels fluctuate seasonally and geographically due to:  temperature  solar radiation  timing of the growing and dormant seasons  land area
  • 61. 4. Describe a pathway of nitrogen from the atmosphere into the body tissue of an herbivore.
  • 63. 5. Describe how an atom of phosphorus might move from the crystal lattice of a mineral in a rock, through a plant, and into the ocean.
  • 64.  phosphate salts are release from rocks through weathering, leaching, erosion, mining or agricultural fertilizers usually dissolved in water  dissolved phosphate being absorbed by plants  animals absorb phosphates by eating plants or plant-eating animals  when animals or plants die, phosphates returns to the soil or ocean (source: http://www.lenntech.com)
  • 65. 6. List and describe three different inputs of sulfur into the atmosphere.
  • 66. Sulfur enters the atmosphere from several sources: 1. combustion of fossil fuels 2. volcanic eruptions 3. exchange at the surface of the oceans
  • 67. 7. Describe how ozone is formed at different levels of the atmosphere and how biological organisms are affected by ozone.

Hinweis der Redaktion

  1. A variety of environmental factors (climate, radiation) influence productivity Mean annual temperature: higher temp also means longer growing season - both higher rates and more days over which there is photosynthesis The higher the rainfall more water available for transpiration, stoma can remain open and photosynthesis can take place longer. Interaction of temperature and moisture; warmer temperature increase evapotranspiration, there increase water demand if not enough water, productivity will be low Need both high temperature and high moisture for highest production
  2. In addition to climate, the availability of essential nutrients required for plant growth has a direct effect on ecosystem productivity by influencing nutrient uptake, photosynthesis and plant growth John Pastor, U of Min in Blackhawk Island, Wisconsin, clearly show relationship between nitrogen availability and aboveground primary productivity
  3. Most productive waters of the ocean are the shallow waters of the coastal environments: 1 shallow waters allow for greater transport of nutrients from bottom sediments to surface waters than deeper waters. (2) coastal regions receive a lot of inputs from terrestrial ecosystems 3. since light is a limiting productivity factor in aquatic ecosystems, open oceans generally have deeper depths thus photosynthetic rate declines as light intensity decreases.
  4. Primary production is a limiting factor to secondary production. Secondary production depends on primary production for energy Herbivore biomass and consumption of primary productivity by herbivores increase with primary productivity
  5. Orange arrows linking trophic levels represent the flow of energy associated with ingestion. The blue arrows from each trophic level represent the loss of energy through respiration. The brown arrows represent the combination of dead organic matter (unconsumed biomass) and waste products (feces and urine)
  6. In most terrestrial and shallow-water ecosystems, with high standing biomass and relatively low harvest of primary production by herbivores, the detrital food chain is dominant. In deep-water aquatic ecosystems, with their low standing biomass, rapid turnover of organisms, and high rate of harvest, the grazing food chain may be dominant.
  7. Energy decreases in each successive trophic level Ecological rule of thumb is that only 10 percent of the energy stored as biomass in a given trophic level is converted to biomass at the next higher trophic level Trophic efficiency - ratio of productivity in a given trophic level with the trophic level upon which it feeds P/P, measure of efficiency that is used to describe he transfer of energy between trophic levels
  8. Important consequence of decreasing energy transfers through the food web is a corresponding decrease in the standing biomass of organisms within each successive trophic level Exception in some lakes and seas
  9. Most essential nutrients are recycled within the ecosystem Plant uptake of nutrients in mineral or inorganic form, Incorporation (nitrogen into enzymes, proteins) Retranslocation (from leaves about to be shed) up to 70% can be recovered
  10. Bacteria and fungi secrete enzymes into plant and animal tissues to break down the complex organic compounds Fragmentation of leaves, twigs and other organic matter. Heterotrophs function as decomposers by digesting food, break down organic matter, alter structurally and chemically, and release it partially in form of waste products.
  11. Temperature & moisture greatly influence microbial activity. Low temperatures and humidity reduce or inhibit microbial activity. Alternate wetting and drying and continuous dry spells tend to reduce microflora activity and populations Decomposition rates are highest in warm, wet climates. The decline in decomposition rate from north to south is a direct result of changes in climate primarily temperature Diurnal temperature changes effect release of Co2 by respiring decomposer organisms
  12. Absence of fungi (they require oxygen) hinders the decomposition of lignin compounds especially among plants In mud and sediments of aquatic habitats where oxygen levels can be extremely low, anaerobic carry out most of the decomposition
  13. Diagram illustrating the exchanges between litterbag and soil in a standard litterbag experiment (litterbag- approach use to study dead plant tissues) Decomposer organisms (bacteria and fungi) colonize the plant litter. As litter is consumed, a significant proportion of carbon is respired, and nutrients bound in organic matter are mineralized and released to the soil. To convert plant carbon to microbial biomass, mineral nutrients are taken up in the process of immobilization. The difference in the rates of mineral nutrient release (mineralization) and immobilization is the rate of net mineralization. As time progresses, the residual organic matter in the litterbag is composed of a growing proportion of microbial biomass as the original plant material is consumed, respired and converted into microbial biomass.
  14. Immobilize- keeping it from there in an available form, sort of a mineral reserve During decomposition, not all nutrients will be mineralized in simple inorganic ion form “whatever will be immobilized today will at some point in the future will be mineralized”
  15. Dead leaf material’s nitrogen content 0.5% to 1.5% Nitrogen exists in many forms in the soil and is essential for plant growth and development. Most of the nitrogen found in the soil is in numerous different organic forms. However, plants are unable to use organic forms of nitrogen. Normal, rather complex processes in the soil convert nitrogen from organic forms into ammonium. How can it go above 100%, bacteria/fungi have nitrogen in their own cells, plus they take up what they are breaking down; nitrogen content much higher in decomposers than in plant material
  16. in aquatic systems, the photic zone may be separated from the benthos (where most decomposition goes on) thus, in aquatic ecosystems, the mineralization of nutrients may not get to the primary producers immediately
  17. Differences in nutrient cycling between terrestrial and open-water aquatic ecosystems The two zones not linked in deeper waters: physical separation is a major controlling factor controlling the productivity of open-water ecosystems
  18. With the breakdown of the thermocline and mixing of the water column (turnover), nutrients are brought up from the bottom to the surface water. With the onset of spring, increasing temperatures and light in the epilimnion give rise to a peak in productivity due to the increased availability of nutrients in the surface waters. As the spring and summer progress, the nutrients in the surface water are used, reducing the nutrient content of the water and subsequent decline in productivity occurs.
  19. Flowing water has spatial component Nutrient spiraling Jack Webster (1975) was the first to point out that because nutrients in streams are subject to downstream transport, there is little nutrient cycling in one place. Water currents move nutrients downstream. Webster suggested that rather than a stationary cycle, stream nutrient dynamics are better represented by a spiral. He coined the term nutrient spiraling to describe stream nutrient dynamics As an atom of a nutrient completes a cycle within a stream, it may pass through several ecosystem components such as an algal cell, an invertebrate, a fish, or a detrital fragment. Each of these ecosystem components may be displaced downstream by current and therefore contribute to nutrient spiraling. The length of stream required for an atom of a nutrient to complete a cycle is called the spiraling length Tight spiral- shorter distance of spiral ex. dead leaves & other debris being physically held in place long enough to allow organisms to process the organic matter Open spiral- longer distance ex. Organisms that shred and fragment organic matter can open the spiral by facilitating the transport of organic materials downstream
  20. Upwelling occurs in the open ocean and along coastlines. The reverse process, called “downwelling,” also occurs when wind causes surface water to build up along a coastline and the surface water eventually sinks toward the bottom.
  21. Water that rises to the surface as a result of upwelling is typically colder and is rich in nutrients. These nutrients “fertilize” surface waters, meaning that these surface waters often have high biological productivity.  Therefore, good fishing grounds typically are found where upwelling is common.
  22. In a gas cycle elements move through the atmosphere. Main reservoirs are the atmosphere and the ocean.• In a sedimentary cycle elements move from land to water to sediment. Main reservoirs are the soil and sedimentary rocks.
  23. Leaching occurs when water flowing vertically through the soil transports nutrients in solution downward in the soil profile
  24. Stream-water runoff is often greatest after fire because of reduced water demand for transpiration. High nutrient availability in the soil, coupled with high runoff, can lead to large nutrient losses from the ecosystem
  25. At daylight when photosynthesis begins, plant starts to withdraw CO2 from the air, by afternoon when temperature and relative humidity decreases, rate of photosynthesis declines, CO2 in the atmosphere increases & by sunset, photosynthesis stops, respiration increases therefore atmospheric level of CO2 sharply increases. Same thing happens in aquatic ecosystems
  26. With the onset of the growing season when the landscape is greening, the atmospheric concentration begins to drop as plants withdraw CO2 through photosynthesis. As growing season reaches its end, photosynthesis declines, respiration becomes the dominant process.
  27. For molecular nitrogen (N2) to be used by organisms it must be fixed in a process called fixation this is done by high energy fixation in which factors such as lightening provide the high energy needed to combine nitrogen with the oxygen and hydrogen of water, the second method of fixation is biological fixation which is accomplished by different kinds of micro organisms such as bacteria. Nitrogen is also freed up for use by other organisms by the breakdown of dead organic material in a process called mineralization. In terrestrial ecosystems nitrogen is taken up (assimilation) by plants in the form of ammonia and nitrates, the plants then convert them into amino acids. Herbivores then eat these plants, which convert the obtained nitrogen into different types of amino acids.
  28. The sulfur cycle has both sedimentary and gaseous phases. In the long-term sedimentary phase, sulfur is tied up in organic and inorganic deposits released by weathering and decomposition, and carried to terrestrial ecosystems in salt solution. The gaseous phase of the cycle permits sulfur circulation on a global scale. Combustion of fossil fuels like gasoline Volcanic eruption of Mt. Pinatubo where it greatly increased the sulfuric level of the atmosphere Oceans are a large source of aerosols that contain sulfate but most are redeposited in the ocean as precipitation and dryfall- Dimethylsulfide is the major gas emitted from the oceans
  29. Ozone (O3)- an ambivalent atmospheric gas At different atmospheric levels: Stratosphere- shields the planet from UV light; cycling reaction requiring sunlight maintains ozone in this level Troposphere- born from the union of nitrogen oxides w/ oxygen in the presence of sunlight Ground level- a damaging pollutant, cutting visibility, irritating eyes and respiratory systems, injuring or killing plant life