Changes in ecosystem structure and dynamics are influenced by geological and meteorological events.
Significant geological events include:
Continental drift: the movement of Earth's continents.
Ice ages: prolonged periods of cold affecting species distribution.
Mass extinctions: devastating losses of biodiversity.
Important meteorological events include El Niño phenomena that affect global climates cyclically every 5 to 8 years.
Pangaea: 250 million years ago, Earth was one supercontinent known as Pangaea.
By 100 million years ago, Pangaea split into Laurasia and Gondwana.
Laurasia formed North America, Europe, Asia; Gondwana formed South America, Africa, Antarctica, Australia.
The historical connections among continents help explain modern species distributions.
Example species distributions:
North America, Europe, Asia share closely related species of elk, bison, and trees (maple, oak).
Unique diversity of marsupials in Australia, due to long-term isolation allowed for species like kangaroos and koalas to evolve.
Climate Change Effects:
Continental drift caused changes in climates affecting ecosystem types.
Example: Antarctica was once near the equator, supporting lush forests; now it has a tundra ecosystem at the poles.
Ice ages led to glaciers advancing southward into regions like Canada and parts of the U.S.
Glaciers eliminated existing ecosystems, killing plants and animals.
As the planet warmed, glaciers receded, uncovering land for colonization:
Plants with wind-blown seeds could quickly occupy bare soil.
Animals, like squirrels, help disperse tree seeds northward, allowing gradual tree expansions.
Ecological succession occurred as species slowly migrated northward.
Case Studies:
Pollen samples from lake sediments help trace the historical distribution of tree species, revealing migration patterns over thousands of years.
Example: Pine trees expanded their northern limit over 5000 years; hickory trees took 7000 years to shift their distributions northward.
Ecosystems shifted as glaciers retreated, transitioning from tundra and coniferous forests to temperate deciduous forests.
Mass extinctions, defined as events where at least 75% of species were lost within two million years, have shaped ecosystems:
Five significant mass extinction events occurred, driven by climatic shifts, ice ages, volcanism, and asteroid impacts.
Adaptation challenges faced by species during these periods led to widespread extinctions.
Despite an estimated 4 billion species existing over Earth's history, approximately 99% have gone extinct.
Examples of past extinctions include:
Large mammals like woolly mammoths and saber-toothed cats in North America around 12,000 years ago, likely due to a mix of human influence and climatic changes.