LECTURE 28 - Assemblages & Ecosystems Flashcards

1
Q

communities def

A

Communities: Two or (usually) more species that occur together in
space and time

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2
Q

assemblages def

A

Assemblages? Less well defined, but can be taken simply as a
group of species that live together with no assumptions made about
how or whether they interact with each other

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3
Q

communities over time

A
  • Stable communities maintain consistent species richness & composition but they are an exception as change in species composition is the norm in nature
  • Change is driven by local colonisations (new arriving in the are) and extinctions of species (old disappearing or dying out)
  • Ecologists often use models to understand how communities change. One common model is ecological succession, which describes how different species replace each other over time in a predictable pattern following a disturbance such as the ecological succession.
  • When a disturbance, like a wildfire or a volcanic eruption, affects an ecosystem, there are predictable patterns of how species recolonize and establish themselves. This process of recovery follows a sequence that ecologists study.
  • New communities are being assembled by human activity / Human activities, such as urbanization, deforestation, and the introduction of non-native species, can disrupt natural ecosystems. This can lead to the assembly of new, often human-altered, communities.
  • New communities are often homogeneous in many parts of the world –
    ‘biotic homogenisation’ / Due to human activities like globalization and the spread of invasive species, some communities around the world are becoming more similar or “homogeneous.” This can lead to a loss of biodiversity as unique local species are replaced by a smaller set of widespread species.
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4
Q

ecological succession

A

Ecologists often use models to understand how communities change. One common model is ecological succession, which describes how different species replace each other over time in a predictable pattern following a disturbance

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5
Q

succession in general

A

Succession - general
* Early ideas related to forests: tree falls down, creating gap for light [One common starting point is when a large tree falls, creating an opening in the forest canopy. This opening allows more sunlight to reach the forest floor.]

  • Light unsuitable for certain species (esp. shade-tolerant), creates high
    quality environment for other species
    [The increased sunlight in the gap can be unsuitable for some tree species that are adapted to shade. However, it creates a favorable environment for other plant species that require lots of light. So, the change in light conditions creates opportunities for different types of plants to grow.]
  • Changes in species composition and abundance, growth rates in lower canopy and ground level strata
    [With more light, the plant species composition changes. Shade-tolerant species might decline, while light-loving species become more abundant. This affects the overall structure of the forest, including plants at different heights, like the lower canopy and the forest floor.]
  • Dominant species in system change over time.
    [Over time, the plant species that dominate the area can change. Initially, the gap might be filled with fast-growing pioneer species. As the forest matures, other, more shade-tolerant species might become dominant. This shift in dominant species characterizes different stages of succession.]
  • Various biogeochemical
    processes associated with the presence of certain species also
    change
    [Different plant species have different effects on the soil and nutrient cycling. As the dominant plant species change, so do the biogeochemical processes in the ecosystem. For example, some plants might fix nitrogen in the soil, while others do not. These processes can influence nutrient availability for other plants and organisms.]
  • New dominant species move in [As succession progresses, new species take over and become dominant. This can lead to further changes in the environment, creating a dynamic process of ecological change.]
  • Equivalent changes often seen with animals, fungi etc
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6
Q

pioneer species

A

Pioneer Species: the first plants to colonize a previously uninhabited or disturbed area, such as a newly formed volcanic island, a cleared field, or a recently abandoned construction site.

  • grow in sun : prefer / tolerate full sunlight
  • fix nitrogen : Some pioneer species have the ability to fix atmospheric nitrogen into a form that plants can use. This is an essential nutrient for plant growth, and these species help enrich the soil with nitrogen.
  • good dispersal : typically have effective mechanisms for dispersing their seeds over long distances. This helps them reach new, open areas and establish themselves quickly.
  • small seeds : can be easily transported by wind, water, or animals.
  • rapid growth
  • short generation time/ short life cycle
  • poor competitors : ay not compete well with other, more established plants because they are specialized for colonizing open environments.
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7
Q

climax species

A

Climax species are plants that dominate and thrive in the later stages of ecological succession when the environment has become more stable and mature.

  • shade tolerant
  • slow growth
  • long-lived
  • good competitors
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8
Q

types of sucession

A

primary
secondary

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9
Q

primary succession

A

the process of ecological development in an area that initially lacks soil and is devoid of living organisms. It typically occurs in areas that have been completely sterilized or where no life has existed before.
* Bare area without soil
e.g. sand-dune, bare rock

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10
Q

secondary succession

A

the process of ecological development in an area that occurs in habitats that have already been influenced by living organisms and have some existing soil. This type of succession typically happens in areas that have been disturbed or altered by events like fires, logging, or abandoned farmland. Secondary succession is a process where an ecosystem regenerates and gradually returns to its previous state.

  • In a habitat modified by other species
    e.g. forest gaps, abandoned agricultural fields
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11
Q

models of succession

A

Models of succession
Facilitation
* early arriving species make environment more favourable for later species [ pioneer species establish themselves and die off, they contribute organic matter to the soil.]
Tolerance
* neither negative nor positive interactions between early
and late species
Inhibition
* early species inhibit later species
ME : early-arriving species inhibit the establishment of later-arriving species. This inhibition occurs because the early species dominate resources or alter conditions in a way that makes it challenging for other species to take hold.
As time progresses, conditions might not become more favorable for late-successional species. Instead, the early species maintain their dominance, and the community remains relatively stable with limited species turnover.

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12
Q

resilience

A

the ability of a natural community or ecosystem to recover and return to a stable state after it has been disturbed. [measure of how long it takes for nature to bounce back to a balanced condition after something disrupts it.]

When studying resilience and succession, it’s essential to have clear criteria for defining the conditions before and after a disturbance. These criteria help scientists measure and understand the changes that occur.

For example, in Australia, a common criterion used to define pre-disturbance conditions is “before 1788.” This means that researchers often use the state of ecosystems and communities as they existed before European colonization as a reference point for understanding natural conditions.

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13
Q

PROBLEMS with the “before 1788” criteria

A

Problems with the ‘Before 1788’ Criterion:

Using the “before 1788” criterion in Australia has its challenges. It assumes that the state of ecosystems before European settlement is the ideal or natural condition. However, this assumption can be problematic for several reasons:
a. Indigenous land management practices were in place before 1788, which means that ecosystems were already influenced by human activity.

b. It doesn’t account for the fact that ecosystems change naturally over time.

c. It doesn’t consider the dynamic and shifting nature of ecosystems or the impacts of other disturbances like climate change.

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14
Q

Ecosystems def

A

The community of living organisms considered in
conjunction with the abiotic components of their
environment, interacting as a system

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15
Q

Biogeochemical cycles

A

how elements and compounds essential for life, like C, N, P, S move through living organisms, the atmosphere, the Earth’s crust (geology), and back into living organisms. These cycles involve both (bio), (geo), and (chemical) processes.

  • Energy flows through the biosphere
  • Materials are recycled [Unlike energy, which flows in one direction, materials (elements and compounds) are recycled in ecosystems. For example, carbon, nitrogen, and other elements are used by living organisms, returned to the environment through processes like decomposition, and then reused by other organisms.]
  • Ecosystem productivity is controlled by efficiency of recycling as well as by energy available
  • Materials transported in the atmosphere (H2O, C, N, S)–> global cycles [These elements move through the Earth’s atmosphere, and their distribution and movement have a global impact on climate, ecosystems, and the environment.]
  • Phosphorus, potassium, calcium and magnesium move through
    soil–> local ecosystem cycles
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16
Q

THE WATER CYCLE

A
  • ~ 97% of water on earth is in the
    oceans
  • Processes of
    1. convection : warm air rises, gets cooled and then descends, contributing to the cycle
    2. precipitation : release of water from the atmosphere in the form of rain, snow, sleet, or hail. Precipitation is how water returns to the Earth’s surface
    3. transpiration
    4. respiration
    –> move water around the cycle
  • ~ 3% of total water is relatively
    inaccessible, in icecaps, glaciers and as
    deep groundwater
  • Within the scale of local ecosystems,
    water behaves more like energy
    because it effectively flows through
    and is not recycled locally
17
Q

nitrogen cycle

A

Abundant in atmosphere, 78%

  • Plants cannot absorb atmospheric
    nitrogen
    –> bsorbed as ammonium or nitrate
    after fixation of nitrogen by
    symbiotic bacteria, or in soil
    solution
  • Denitrifying : This is when certain types of bacteria convert nitrates (a form of nitrogen that plants can use) back into gaseous nitrogen. This gaseous nitrogen can then return to the atmosphere, completing the cycle.
  • Electrical storms also fix nitrogen [ightning can convert atmospheric nitrogen into forms that can be used by plants and organisms, making it available in the soil.]
  • Nitrogen becomes limiting if
    microbial activity is inhibited
18
Q

carbon cycle

A
  • Most carbon is locked up in
    earth’s rocks as carbonate (and
    also fossil fuels)
  • The most active pool is carbon
    dioxide, 0.04 per cent of the
    atmosphere (… and increasing)
  • CO2 is used in photosynthesis,
    released during respiration
  • Large amounts of CO2 are
    dissolved in the ocean
  • Burning fossil fuels returns CO2 to
    the atmosphere faster than it can
    be cycled
    –> global warming
  • Regulation by animal : [through their respiration and consumption of plant matter. However, their impact on the carbon cycle is relatively small compared to the larger processes like photosynthesis, respiration, and the exchange of carbon between the atmosphere and the oceans.]
19
Q

phosphorus cycle

A
  • Essential to all life, in ATP
  • Not common in earth’s crust or in
    atmosphere
  • Taken up by plants as phosphate
    from sparingly soluble soil storage
    pool
  • Australian flora are well adapted to
    low P, and efficient at recycling
    phosphorus
  • Symbiosis between plant roots and
    mycorrhizal fungi enhances the
    phosphorus supply