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Biome
One of the globes’s major ecosystem types, classified according to the predominant vegetation (for terrestrial) and the physical environment (for aquatic) present
are also characterized by the adaptations of organisms to that particular environment
Climate
The long-term, major weather conditions in an area
has major influence on the distribution of terrestrial biomes
Climate abiotic factors
1) temperature
2) Precipitation
3) Sunlight
4) Wind
Climograph
Plots the annual mean temperature and precipitation for a particular region
Tropical forests
Near equator
High temps with low seasonality
High rainfall
Broadleaf evergreen or deciduous trees
Highest animal diversity
Savannas
1) Near equator
2) High temps with more seasonality
3) Low rainfall
4) Scattered trees, grasses, forbs
5) Fire adapted
Chaparral
1) Midlatitude coasts
2) Cold temps with hot summers
3) Low rainfall with high seasonality
4) Small trees
5) Fire adapted shrubs
Tundra
1) The Arctic and very high mountaintops
2) Very low temps
3) Low to moderate precipitation
4) mosses, grasses, forbs, lichens
Temperate broadleaf forests
1) Midlatitudes
2) Cold winters and hot, humid summers
3) Moderate precipitation all year
4) Deciduous trees in North America
Temperate grasslands, deserts, and Northern coniferous forests (taiga)
Are three terrestrial biomes common in New Mexico
Ecotone
An area of integration between biomes
Oceans
The largest biome, covering 75% of Earth surface
Photic zone
Sufficient light for photosysthesis
Aphotic zone
Little light can penetrate
Pelagic zone
Open water colum
Benthic zone
On the bottom, including organic and inorganic sediments and the benthos
Benthos
Community of organisms
Littoral zone
Near shore
Limnetic zone
Away from shore
Estuary
The transition zone between rivers and the ocean
Thermocline
A narrow layer of abrupt temperature change that separates warm, upper layer from cold, deep water
Oligotrophic lakes
Nutrient poor and oxygen rich
Eutrophic lakes
Are nutrient rich and oxygen poor
Microbiome
The collection of microorganisms living in and on the body
can differ based on diet, disease, age, host environment, host phylogeny and body region
Biodiversity
Describe the total variety and variability of life on Earth
considered at three levels
Genetic diversity
Species diversity
Ecosystem diversity
Genetic diversity
Comprises variation within individuals within populations, and between populations
the variation necessary for adaptive evolution
Species Diversity
Includes the total number of species an their relative abundances in an ecosystem and across the biosphere
endangered species
Threatened species
The total variety of different organisms present
species richness
Relative abundance
Endangered species
Are in danger of extinction throughout all or much of their ranges
Threatened species
Likely to become endangered in the future
Ecosystem diversity
The variety of ecosystems on earth, including the interactions between organisms and their environment
Species richness
The number of different species in a community
Relative abundance
The proportion of individuals in the community represented by each species
Species area curve
The pattern that the larger the geographic area of a community, the more species it has
Dispersal
Mobility of species can limit diversity in come areas
Biogeography
The study of the geographical distributions of species and cosystems across geographic space and geological time
Cosmopolitan
Wide ranging
They may be habitat or diet generalists, or parasites that are host generalists
Endemic species
Are found in one are and nowhere else in the world
Enderism
Mountains and islands then ti restrict ranges and promote
Community science (citizen science)
Scientific research conducted by members of the public
iNaturalists
(Started in 2008) allows anyone with a smart phone to upload photos or audio of species observed in nature
Global Biodiversity Information Facility
Aggregators that museums send specimens data
Primary Producers
(Autotrophs) ultimately support all other tropic levels
Detritus
Nonliving organic material such as dead organisms and leaves
Detritivores or decomposers
Digest the dead materials and nutrients can be cycled back to producers and consumers
Net Primary Production
The gross primary production minus the energy used by the autotrophs for their own cellular respiration
NPP= GPP - Ra
Net Ecosystem Production
The gross primary production minus the total respiration of all organisms, including autotrophs and heterotrophs in the system
NEP = GPP - Rt
Biophilla
Hypothesis says humans have a sense of connection to nature and all forms of life
Biomass
G
Introduced species
K
Ecosystem services
Include all processes through which natural ecosystems help sustain human life
List the ecosystem services
1) purify air and water
2) detoxify and decompose wastes
3) reduce impacts of flooding
4) control pests
5) create and pressure soils
6) pollinate crops
Bioremediation
Involves using organisms such as prokaryotes, fungi, or plants to detoxify polluted ecosystems by removing harmful substances
Biological augmentation
Uses organisms to add essential materials to be degraded ecosystems
Law of conservation of mass
States that matter cannot be created or destroyed
Biogeochemical cycle
Describes the path an element takes as it moves between abiotic and biotic components
Decomposers
growth is controlled by temperature, moisture, and nutrients
Reservoirs
Where chemical elements are found in and move between
Major: ocean (97%)
glaciers and polar ice caps (2%)
lakes, rivers, groundwater (1%)
Include: fossil fuels, soils, oceans, organisms, atmosphere, and sedimentary rock
Atmosphere: N2 gas (80%)
Limiting nutrient
In plants nitrogen is essential for amino acids, proteins, and nucleic acids
Nitrogen fixations
2 is converted to biologically usable forms by fungi and bacteria
Nitrification
The conversion of ammonia to nitrite and nitrate
Denitrification
The conversion of nitrite and nitrate into N2
Eutrophication
A process in which nutrient concentrations increase and cause increased growth of algae and Cyanobacteria
Fossil
The preserved remains of a once-living organism, often formed when minerals fill the spaces within organic material and create a cast
Trace fossils
Preserve the evidence of life, but not the organism itself (footprints, burrows)
Strata
The position of fossils within sedimentary rock layers that provides a relative age
Radiometric dating
Used to determine the age of rocks and fossils by measuring the abundance of radioactive isotopes within them
Half life
Time require for 50% of the isotope to decay
Geological record
A standard time scale dividing Earth’s history into four eons and further subdivisions
Precambrian
The first three eons that lasted approximately 4 billion years
1) Hadean Eon
2) Archaean Eon
3) Proterozoic Eon
Phanerozoic Eon
the fourth and current eon that includes the last 541 million years
Split into three eras ( which are split into periods then epochs)
1) Paleozoic era
2) Mesozoic era
3) Cenozoic era
Paleozoic Era
541 to 252 MYA
Starts with the Cambrian Explosion
major radiations of fungi, arthropods, mollusks, fishes, early tetrapods, conifers
Colonization of land by fungi, plants, giant arthropods, tetrapods
Formation of ecosystems including coral reefs, soils, forests, coal beds
Cambrian Explosion
A sudden increase in diversity of lifeforms, including the first appearance of all modern animal phyla
Tetrapods
Four limbed vertebrates
The Great Dying
Mass extinction in the Permian period and the largest recorded extinction event
Permian extinction
Claimed 96% of marine animal species, drastically altered ocean life, and wiped out a substantial number of insect groups
Mesozoic era
252 to 66 MYA
“The age of the reptiles”
Begins with a period of recovery and major faunal shifts
Appearance of major modern groups including angiosperms, insects, mammals, birds
Major radiations of chordates including dinosaurs, crocodiles, turtles, synapsids (ancestors of mammals), and pterosaurs (first with powered flight)
Cretaceous extinction
Wiped out >50% of marine species and major terrestrial animals including dinosaurs (except birds)
Cenozoic Era
66 MYA to present
“age of mammals”
Begins with a period of recovery ad major faunal shifts
Diversification of grasses, mammals, birds, and evolution o modern genera and species
The Great American Interchange occurred 2.7 million years ago when the isthmus of Panama arose and Nearctic and Neotropical fauna mixed
Cenozoic era
Ends with quaternary period, including two epochs
1) Pleistocene
2) Holocene
Pleistocene epoch
2.6M to 11,700
glacial-interglacial cycling: alternating periods of the planet cooling (ice ages) and warming
Anatomically modern humans spread around the globe
Megafaunal extinctions around the globe, debated whether caused by climate change, human hunting, or both
Holocene Epoch
11,000 ya to present
all of written human history
Industrialization and human population increase in last ~200 years
Hadean Eon
4.6 to 4 billion years ago
water brought from asteroids and comets begins to accumulate
Surface solidifies into plates sitting on top of magma, moving around via currents
Organic compounds are interpreted as the first evidence of life on earth
Archaean Eon
4 to 2.5 billion years ago
first fossil evidence of life
Oxygen producing bacteria are present and atmospheric oxygen begins to increase
Stromatolites
Layered rocks formed by prokaryotes
Proterozoic Eon
2.5 billion to 541 million years ago
oxygenation of the atmospheric leads to a shift from anaerobic to aerobic lifeforms
Eukaryotic life (cells and nuclei) originates 1.8 billion years ago and becomes dominant
multi cellular eukaryotes emerge 1.3 billion years ago
Precambrian
By the end, fund consisted of soft-bodied organisms with tissues that do not resemble most of modern lifeforms
Speciation rate
Number of species produces in a period of time, also called origination)
Extinction rate
Number of species lost in a period of time
Plate tectonics
How continents are part of large fragments of earths crust, floating on hot mantle below
Continental drift
Currents in the mantle cause plates to move over time
Pangaea
Supercontinent at the end of Paleozoic era
Laurasia
Northern landmass by mid-Mesozoic era
Gondwana
Southern landmass
Mass extinction
When large numbers of species become extinct worldwide at a rate exceeding the typical average rate
Adaptive radiations
The loss of species in ecological roles in which a group diversifies to fill empty niches
Anthropocene
Been proposed as a new geological epoch that highlights the significant impacts humans are having on earth
Threats to biodiversity
1) Habitat loss
2) Over harvesting
3) Global change
Habitat loss
By far the greatest threat to biodiversity is habitat loss, fragmentation, and alteration
Reasons: agriculture, forestry, mining, urban development, pollution, dams and reservoirs, ocean trawling, climate change
Effects: extinction, deceases in population size, genetic diversity
Possible solutions: shift towards plant-based diet, protected lands, restoration, land using planning
Overharvesting