• Skip to primary navigation
  • Skip to main content
  • Skip to footer
  • About
  • Image & Use Policy
  • Translations
  • Glossary

SUPPORT UE

  • Email
  • Facebook
  • Twitter

UC MUSEUM OF PALEONTOLOGY

UC Berkeley logoUC Berkeley

Understanding Evolution

Understanding Evolution

Your one-stop source for information on evolution

Understanding Evolution

  • Home
  • Evolution 101
    • An introduction to evolution: what is evolution and how does it work?
      • 1_historyoflife_menu_iconThe history of life: looking at the patterns – Change over time and shared ancestors
      • 2_mechanisms_menu_iconMechanisms: the processes of evolution – Selection, mutation, migration, and more
      • 3_microevo_menu_iconMicroevolution – Evolution within a population
      • 4_speciation_menu_iconSpeciation – How new species arise
      • 5_macroevo_menu_iconMacroevolution – Evolution above the species level
      • 6_bigissues_menu_iconThe big issues – Pacing, diversity, complexity, and trends
  • Teach Evolution
    • Lessons and teaching tools
      • Teaching Resources
      • Image Library
      • Using research profiles with students
      • Active-learning slides for instruction
      • Using Evo in the News with students
      • Guide to Evo 101 and Digging Data
    • Conceptual framework
      • Alignment with the Next Generation Science Standards
      • teach-evo-menu-icon
    • Teaching guides
      • K-2 teaching guide
      • 3-5 teaching guide
      • 6-8 teaching guide
      • 9-12 teaching guide
      • Undergraduate teaching guide

    • Misconceptions about evolution

    • Dealing with objections to evolution
      • Information on controversies in the public arena relating to evolution
  • Learn Evolution

Home → Putting it in perspective: Climate change yesterday and today

    Putting it in perspective: Climate change yesterday and today

    We all know that things change — but in terms of Earth’s history, things have really changed. Life has originated, evolved, diversified, and, in most cases, gone extinct. Continents have arisen, broken apart, and collided. Mountain ranges have formed and eroded. Even the make-up of the atmosphere has changed.

    Today, carbon dioxide levels are rising — but how do today’s levels compare to those of the past? These snapshots will help put it in perspective:

    • 430 million years ago: When most life lived in the oceans and plants were first invading the land, carbon dioxide levels were ten to twelve times higher than today!

    Illustration of what the landscape might have looked like on Earth 430 million years ago when most life lived in the oceans and plants were first invading the land, carbon dioxide levels were ten to twelve times higher than today.

    • 300 million years ago: After land plants diversified, lush forests and diverse plant communities crept across the Earth. These plants sucked up carbon dioxide from the atmosphere, leading to carbon dioxide levels slightly lower than today.

    Illustration showing what Earth might have looked like 300 million years ago when land plants diversified, lush forests and diverse plant communities crept across the Earth.

    • 175 million years ago: The “Age of the Dinosaurs” was generally warm and humid, with carbon dioxide levels three to five times higher than today.

    Illustration showing what the landscape on Earth might have looked like 175 million years ago during the "Age of the Dinosaurs" which was generally warm and humid, with carbon dioxide levels three to five times higher than today.

    • 140 million years ago: Flowering plants first evolved and diversified in an environment that probably had moderately high carbon dioxide levels — perhaps twice those of today.

    Illustraiton showing what Earth might have looked like 140 million years ago when flowering plants first evolved and diversified.

    • 65 million years ago: Since the non-avian dinosaurs went extinct, carbon dioxide levels have been steadily decreasing — that is, up until the recent past…

    So in comparison to much of Earth’s history described above, modern carbon dioxide levels are relatively low. However since the industrial revolution, humans have been releasing greenhouse gasses in mass quantities, increasing the level of carbon dioxide in the atmosphere. Currently, human activities are causing carbon dioxide levels to change more rapidly than volcanoes, asteroids, or anything else in Earth’s 4.5 billion year history. In fact, if we keep to our current practices, we will cause carbon dioxide levels to double by the end of this century — a level of carbon dioxide unprecedented for all of human existence and the past 50 million years!

    • More Details

    Learn more about greenhouse gases on the Understanding Global Change site.

    Footer

    Connect

    • Email
    • Facebook
    • Twitter

    Subscribe to our newsletter

    Teach

    • Teaching resource database
    • Correcting misconceptions
    • Conceptual framework and NGSS alignment
    • Image and use policy

    Learn

    • Evo 101
    • Evo in the News
    • The Tree Room
    • Browse learning resources
    • Glossary

    Copyright © 2025 · UC Museum of Paleontology Understanding Evolution · Privacy Policy

    We use cookies to see how our website is performing. We do not collect or store your personal information, and we do not track your preferences or activity on this site.Ok