Flora Flashcards
Australia’s Biodiversity: A mega-diverse country
- 8% of World’s species
* Many species endemic
Australia’s Fauna
- Bird
- Lizard
- Mammals
Australia’s Unique Flora
Flowering plants•> 21,000 species•> 90% of Australian species are endemic
What was the origin and history of this unusual Australian biota?
They observed that related plants and animals occurred also in the southern hemisphere, ‘linking’the continents.
Where plants lived in the past -clues to history
- showed evidence of ancient forests
- included leaves, stems, roots of seed fern Glossopteris
- Permian age (286-248 mya)
- Dominant trees
- Grew in swamps that formed coal deposits
- Fossils also in India, South America, South Africa & Australia (many species)
Explanation of a southern biota -its fossils and current distribution patterns
- Old idea(up to 1960’s): recent long distance dispersal over waterways land bridges that connected stationary continents, e.g. ratites walked!
- Modern theoryof continental drift -sea floor spreading and plate tectonics explain old union of land masses and their later movement apar
Moving continents
- Earth has experienced a number of tectonic cycles of continents coming together and moving apart
- Last major cycle started c. 320 mya, by c. 230 mya continents were coalesced into supercontinent Pangea
- Within Pangea, northern land masses joined to form Laurasia; southern lands formed Gondwana
- Pangea began to break up in mid Jurassic (c. 160 mya)
Gondwana break up
- NZ started separating c. 80 mya
- Australia separated by 35 mya
- South America separated c. 30 mya or later
Example of southern hemisphere distributions
- Bony-tongue freshwater fishes
- Ratites (flightless birds)
- Nothofagus -flowering plant(southern beech trees)
Consequences of drifting northwards Climates
Climate changes
•Warm, humid, rainforests initially widespread
•Circum-polar current: cooling of Antarctica
•Reduced wind-bearing rains over Australia and increased aridity from Oligocene (30 my ago)
•Contraction of rainforest decreased
•Evolution and expansion of more arid-adapted plants, e.g. sclerophylls, and animals adapted to them
Consequences of drifting northwards landform
- Old land surface, little mountain building or volcanic activity
- Weathering during warm-wet periods leached nutrients from soils
- Soils became low in nutrients e.g. Phosphorus
- Drier cooler periods increased wind erosion. Mobile dunes; inland lakes dried up & became salt plains
- Evolution further favouredarid-adapted flora & fauna
Consequences of drifting northwards Fire
- Evidence from charcoal and pollen fossil record
- Infrequent but present in wetter periods
- Caused by lightning, volcanoes
- Increased frequency with aridity
- Rainforest contracted further, sclerophyllsfire-adapted
Pleistocene “Ice ages”
- World-wide fluctuating interglacial(warm) and glacial(cold) periods 2.5 my -present
- Australia warm wet/cool dry periods, virtually no glaciation (ice)
- Mobilisationof sands and expansion of desert regions
- Changes in sea level
Arrival of humans
- Genetic evidence: 50 kya
- Archaeological evidence: 49-65 kya
- Possible indirect evidence: charcoal deposits ?100-120 kya
- Fire-stick farming
Megafaunal extinctions
•Concentrated 35-48 kya
Climate change?Hunting?Human use of fire?
Southwest WA: why is it so rich in endemic species?
-Long history of isolation
-Isolation through marine incursions at times of higher sea levels
-•Periods of high sea level: 42–34, 27–21, 16–14 mya
•Limestone deposits created soil (edaphic) barriers
Isolation through climate
-Patterns of species diversity are shaped by evolution –this is influenced by earth history (including climate & geology)
Important of AUSTRALIAN RAINFORESTS
- Surviving remnants of Gondwanan flora & fauna
- Provide a glimpse back in time to vegetation of Gondwana
- High conservation value, NE Queensland Wet Tropics World Heritage Area
- Species rich -50% Australian ferns in rainforests
- 13 of the most primitive flowering plant families
- Austrobaileya-pollen similar to oldest angiosperm fossils (120 million years old)
- Animals withprimitive features
Austrobaileya
- Genus of 1 species (A. scandens)
- Usually placed in its own family (Austobaileyaceae)
- has pollen similar to oldest angiosperm fossils (120 million years old)
TROPICAL RAINFORESTS
- Lowland -most species rich
- 100-200 tree species per hectare
- 1000 beetle species per tree
- Many ferns and palms
- Trees with large leaves (>12.5 cm)
TEMPERATE RAINFORESTS
- Fewer species, South, few vines
- Fewer layers, simpler structure
- Smaller leaves (2.5-7.5 cm)
- Cool temperate rainforests in Vic. & Tas. with single species often dominant:
Lowland tropical rainforests
Climate uniformly warm wet
•Rainfall >1800 mm, alt.<1000 m
•Rapid nutrient cycling
•Regional differences in composition
Leaf adaptations in rainforrest
- Large leaves
- Smooth surface and drip tip prevent moisture accumulating & fungal growth
- guttation: Pores on leaf edge drip water -root pressure forces water (& mineral nutrients) up plantWhen humidity high, little evaporation & transpiration stream
- large compound leaves
Compound leaves in rainforests
Can provide good surface area for capturing light, but also light penetration to lower branches
•Can be “cheaper” to produce than branches
Buttress and prop roots
- Structural support -shallow root system (feedingroots near surface)
- ?competition