Biology - Review 10 Flashcards
How is the geological time scale is constructed ?
The geological time scale is constructed using the relative order of rocks in a sedimentary rock sequence, the fossilised remains of ancient animals and plants within the rock strata, and direct dating of rocks using radiometric techniques.
What are the geological time scale divisons?
4 divisions
The largest geological subdivision of the geological time scale is an eon.
Eons are subdivided into eras,
which are further subdivided into periods,
and into still smaller subdivisions called epochs.
What happened in the In the Archaean eon?
Lite first appeared on Earth. Earth’s initial life forms were prokaryotes (bacteria). Stromatolites and other early prokaryotes were Earth’s sole inhabitants for more than 1.5 billion years.
What happened in the In the Proterozoic eon?
- Single-celled and multicellular eukaryotes such as algae (red algae and green algae) appeared.
- The Ediacaran period includes the earliest evidence of multicellular animals called the Ediacaran fauna. These animals were small
- Soft- bodied sea creatures that resemble modern sea jellies and segmented worms.
What were the periods of the Palaeozoic era?
6 periods
- Cambrian period
- Ordovician period
- Silurian period
- Devonian period
- Carboniferous period
- Permian period
What were the periods of the Mesozoic era?
3 periods
- Triassic period
- Jurassic period
- Cretaceous period
What were the periods of the Cenozoic era?
3 periods
- Palaeogene period
- Neogene period
- Quarternary period
Describe
Cambrian period
Cambrian period—a dramatic increase in the number and complexity of marine life forms, including animals with exoskeletons.
Describe
Ordovician period
Ordovician period—the emergence of the first vertebrates, the jawless armoured fishes (ostracoderms).
Describe
Silurian period
Silurian period—the first known air-breathing animals were arthropods: millipedes and centipedes. The earliest arachnids also appeared. Small vascular plants colonised swampy land.
Describe
Devonian period
Devonian period—jawed marine fishes evolved, along with armoured placoderms. ray-finned and lobe-finned fishes and early sharks. One group of finned fishes developed sturdy fins that they were able to support their weight at the edge of the water and led to the evolution of tetrapods.
Describe
Carboniferous period
Carboniferous period—evolution of reptiles from amphibian-like ancestors. Formation of forests dominated by tree forms of spore-bearing vascular plants including lycophytes and sphenophytes.
Describe
Permian period
Permian period—one massive continent called Pangaea formed, reptiles diversified, and a mass extinction event occurred in which up to 90% of species became extinct
Describe
Triassic period
Triassic period—reptiles were the dominant vertebrates. The archosaur reptiles, had diversified into pterosaurs, crocodiles and the earliest dinosaurs. Evidence of the earliest mammals also emerged. Plants included cycads. ferns and Gmgko-like trees.
Describe
Jurassic period
Jurassic period—dinosaurs thrived on a warm, forested Earth giving rise to the first gigantic sauropod and theropod dinosaurs. Mammals had begun to diversify. The oldest bird fossils are from the Jurassic.
Describe
Cretaceous period
Cretaceous period—dinosaur diversity had reached its peak, small primitive marsupials, and insectivores were abundant and widespread. Angiosperms (flowering plants) evolved.
Describe
Palaeogene period
Palaeogene period—mammals evolved into many new species, giving rise to new placental and marsupial species. Birds became abundant and primates evolved.
Describe
Neogene period
Neogene period—the first of the Homo species, Homo hdbilis. evolved.
Describe
Quaternary period
Quaternary period—includes the Pleistocene and Holocene epochs. Climates and sea-levels fluctuated from cold, dry glacial periods and low sea-levels to warm, wetter interglacial periods and higher sea-levels. Some animal species evolved to become giants—the megafauna, which later became extinct.
What is the process of forming impression fossils?
- Death of the organism
- Burial of the organism by sediments
- The weight of many layers of sediments squeezing out water between the particles of sand, silt or mud
- Soft sediments become solid rock—sandstone, siltstone. mudstone or shale (a mixture of clay and silt) as the deposit deepens, and pressure and temperature increase.
How can fossils be dated?
3 methods
Relative dating
Using index Fossils
Absolute dating
How can fossils be dated by Relative dating?
Relative dating is based on stratigraphy, which places the age ot a fossil according to. or relative to, the known age of layers or strata of rock above and below the layer of rock in which the fossil is found