The splitting of Pangaea led to a global rise in biodiversity. As the single supercontinent broke apart, different species were isolated on separate landmasses, leading to the evolution of new species and diverse ecosystems. This increase in biodiversity laid the foundation for the variety of life forms we see on Earth today.
Pangaea was a supercontinent that existed about 335 to 175 million years ago, during the late Paleozoic and early Mesozoic eras. The breakup of Pangaea led to the formation of the continents we have today and shaped the Earth's geological features.
Pangaea began to break apart around 175 million years ago during the Jurassic period. This breakup eventually led to the formation of two separate landmasses known as Laurasia (in the north) and Gondwana (in the south).
Some advantages of Pangaea include increased connectivity of the landmasses which facilitated species migration between continents, creating wider ranges of biodiversity. It also enabled the exchange of flora and fauna, contributing to a richer ecosystem. Additionally, the formation of Pangaea influenced the distribution of resources which could have led to the development of different species with unique adaptations.
Pangaea broke up during the Mesozoic Era, specifically during the Triassic and Jurassic periods, approximately 175 million years ago. This breakup led to the formation of the continents as we know them today.
135 million years later, Pangaea had already split into two supercontinents: Laurasia in the north and Gondwana in the south. This breakup eventually led to the formation of the modern continents we see today.
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Pangaea
Plate tectonics led to the theory of Pangaea.
Global warming is having a massive impact on monkeys in Fiji. Accelerated sea level rise, deforestation, climatic changes and less rainfall has led to a reduced population of monkeys.
Advantage of Pangaea: Increased biodiversity due to species distribution across a vast, connected landmass allowed for unique evolutionary pathways. Disadvantage of Pangaea: Eventually led to mass extinction events as the breakup of Pangaea caused drastic changes in climate and habitats.
Pangaea began to break up during the Triassic period, around 200 million years ago. This breakup eventually led to the formation of the continents we recognize today.
The breakup of Pangaea led to the formation of separate continents, changing ocean currents and wind patterns. This change influenced the distribution of heat and moisture around the Earth, impacting global climate patterns. As continents drifted apart, new climate zones emerged, leading to the development of different ecosystems and climates across the planet.
agriculture
During the time of Pangaea, the climate was generally warm and dry, with forests and deserts covering much of the supercontinent. There were significant climate variations across different regions due to Pangaea's vast size and diverse landscapes. Ultimately, the breakup of Pangaea led to the formation of the modern climate patterns we see today.