EGS Pippin 1. Intro to Biome concept. Flashcards
Overview???
- (), an American ecologist, is sometimes described as the () of the ().
- He focused on how () is ().
- He noted the way plants & animals are () in () across () & () -> developed ()
- () is a () way of looking @ any community to understand what () are () () in that community.
- Robert Whittaker, an American ecologist, is sometimes described as the Godfather of the Biome conept
- He focused on how the diversity of life is distributed.
- He noted the way plants & animals are distributed in particular ways across space & time -> developed Gradient Analysis
- Gradient Analysis is a linear way of looking @ any community to understand what factors are driving composition in that community.
Scientists involved in defining the biome concept
(1). ():
* Point:
* Point:
(2). ():
* Point:
* Point:
(3). ():
* Point:
(4). ().
* Point:
(1). Robert J. Whittaker:
* Defined biomes as large-scale ecological communities w. distinct climate, veg. & animal life
* Know for work on ecological gradients in biomes
(2). Clements (1916):
* First
* Defined biome as a community of plants & animals that occupy a specific geographic area &
* are characterized by distinct climatic conditions
(3). Tansley (1935):
* introduced the term ‘ecosystem’’
* biotic and abiotic factors (soil)
(4) Shelford & Clements (1939):
* further work
Why are biomes useful units?
Means of predicting environmental control of distribution of life
(understanding the mechanisms behind patterns of distribution)
Biomes defined P1/3
- (1) Biomes are () that () major () over (), defined by (), typically (), over () of ().
- (2) While the definition of Biomes has (), they are generally recognised as the () @ the (), mappable at a scale ().
- (3) This scale offers a () view, where () & () areas can be distinguished.
- (1) Biomes are large ecological units that represent major life zones over extensive areas, defined by dominant life forms, typically plants, over long periods of time.
- (2) While the definition of biomes has evolved over time, they are generally recognized as the largest land units @ the continental scale, mappable at a scale no larger than 1:10 Ma
- (3) This scale offers a broad, homogenous view, where typical & less typical areas can be distinguished.
Biomes Defined P2/3
- (4) Biomes are () based on the (), with () made according to ().
- (5) They are (), not ().
- (6) At (), biomes are understood (), driven by () dominant plant cover, with () and () playing secondary roles.
- (4) Biomes are primarily classified based on the dominant plant cover, with secondary distinctions made according to climatic features that most influence the biota.
- They are natural systems, not anthropogenic.
- At macro-scale, biomes are understood mechanistically, driven by factors that determine dominant plant cover, with climate and soil playing secondary roles
Biomes defined P3/3
- (7) With (), such as () & more detailed () like (), () or (), providing further distinctions.
- (8) Despite attempts to simplify, the study of biomes ().
- With functional plant traits, such as macro-growth forms & more detailed ecological characteristics like photosynthetic pathways (C3, C4, CAM), succulence, or sclerophylly, providing further distinctions.
- Despite attempts to simplify, the study of biomes remains complex
Usefulness of Raunkiaer’s Life Form Scheme?
2 points
- Pulls attention away from fixation on specific species → focus on mechanisms of being a specific plant form → understand why they grow where they do.
- They can be understood in relation to their structure, their function, their similarities or dissimilarities in form & function in a way that allows us to understand the factors that allow for growth
Raunkiaer’s Life Form Scheme P1:
(1)
(2)
(3)
(4)
(5)
(6)
(7)
(8)
Just name them
- Phanerophytes
- Chamaephytes
- Hemicryptophyes
- Cryptophytes/Geophytes
- Hydrophytes
- Epiphytes
- Therophytes
- Aerophytes
Raunkiaer’s Life Form Scheme P2:
- (1). Phanerophytes:
- (2). Chamaephytes:
- (3). Hemicryptophytes:
- (4). Cryptophytes/Geophytes:
- (1). Phanerophytes - woody trees, perennial, projecting stems into the air (oak).
- (2) Chamaephytes - woody shrubs w. stems closer to ground (lavender) .
- (3) Hemicryptophytes - smaller, herbaceous plants, biennial or perennial, but near soil (dandelion).
- (4) Cryptophytes/Geophytes - have below ground storage mechanisms (bulbs) (March lilies).
Raunkiaer’s Life Form Scheme P3:
- (5). Hydrophytes:
- (6). Epiphytes:
- (7). Therophytes:
- (8). Aerophytes:
- (5) Hydrophytes - grow completely submerged in water (water lillies)
- (6) Epiphytes - don’t require soil, but grow on plant (orchids)
- (7) Therophytes - annual, opportunistic plants, ruderals, rapid life cycles, lots of seeds (Namaqua Daisies).
- (8) Aerophytes - air plants
Why do we use the 3 photosynthetic pathways?
Way of looking @ landscape full of plants & asking can we draw boundaries anywhere based on how these plants assimilate CO2 & solar energy
The 3 Photosynthetic Pathways:
(1)
(2)
(3)
- C3 pathway
- C4 pathway
- CAM (crassulacean acid metabolism)
The 3 Photosynthetic Pathways P1/3
(1) C3 pathway:
- Point 1:
- Point 2:
- Point 3:
- Point 4:
- Point 5:
- First P; 2. Optimal; _ system; commonality; e.g.s
- First Product = 3-carbon acid
- Optimal @ high CO2 & low temps.
- Older system
- Most common
- Wheat, rice, sunflowers, grass
The 3 Photosynthetic Pathways P2/3
(2) C4 pathway:
- Point 1:
- Point 2:
- Point 3:
- Point 4:
- Point 5:
- First P; 2. Optimal; 3. _ system; 4. commonality; 5. e.g.s
- First Product = 4-carbon acid
- Optimal @ low CO2 & high temps.
- More recent evolutionary system
- Smaller group 3%
- Maize, sugar cane, sorghum, cabbages
The 3 Photosynthetic Pathways P3/3
- CAM (crassulacean acid metabolism):
- Point 1:
- Point 2:
- Point 3:
- Take up energy during the day but only uses it at night
- So they can keep their stomata closed ->
- Water saving, common in arid regions
Effect of Climate Change on Biomes:
- () has gone up and down over the years - ()
- We are () our models in terms of ().
- Some plants may () with higher CO2 levels while others will () with increasing temperatures:
- () favours CO2
- () favours temp
- We have complex models; but ultimately ().
- Carbon has gone up & down over the years - ice core data
- We are outstripping our models in terms of CO2 release.
- Some plants may thrive with higher CO2 levels while others will struggle with increasing temperatures:
- C3 favours CO2
- C4 favours temp
- We have complex models; but ultimately not really sure what will happen long term.