Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Origin of Photosynthesis01:26

Origin of Photosynthesis

Photosynthesis represents a fundamental biological process that transformed Earth's atmosphere and paved the way for complex life. Emerging roughly 3.4–3.8 billion years ago, the earliest photosynthetic organisms harnessed light energy to produce organic compounds. These anoxygenic phototrophs used electron donors like hydrogen sulfide (H₂S) or ferrous iron (Fe²⁺), rather than water, and did not release molecular oxygen (O₂) as a byproduct. Various groups, including green sulfur and purple...

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Tight regulation of Earth's long-term temperature over Phanerozoic time.

Nature communications·2026
Same author

Retracing the Response of Rangifer to Postglacial Climate Change in Arctic Islands.

Ecology and evolution·2026
Same author

Unravelling the drivers of marine biodiversity across the Phanerozoic.

Nature communications·2025
Same author

The role of the North American continent in strengthening the Asian summer monsoon.

Science advances·2025
Same author

Climate drivers and palaeobiogeography of lagerpetids and early pterosaurs.

Nature ecology & evolution·2025
Same author

Landscape-explicit phylogeography illuminates the ecographic radiation of early archosauromorph reptiles.

Nature ecology & evolution·2025

Related Experiment Video

Updated: Jun 29, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Introduction. Pliocene climate, processes and problems.

Alan M Haywood1, Harry J Dowsett, Paul J Valdes

  • 1School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK. a.haywood@see.leeds.ac.uk

Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences
|October 15, 2008
PubMed
Summary
This summary is machine-generated.

Future climate change may be understood by examining past Pliocene climates. This research assesses the reliability of climate models by comparing their predictions to geological records, aiding future climate change understanding.

More Related Videos

Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area
10:14

Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area

Published on: October 25, 2024

Visualizing Oceanographic Data to Depict Long-term Changes in Phytoplankton
08:15

Visualizing Oceanographic Data to Depict Long-term Changes in Phytoplankton

Published on: July 28, 2023

Related Experiment Videos

Last Updated: Jun 29, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area
10:14

Reconstructing Terrestrial Paleoclimate and Paleoecology with Fossil Leaves Using Digital Leaf Physiognomy and Leaf Mass Per Area

Published on: October 25, 2024

Visualizing Oceanographic Data to Depict Long-term Changes in Phytoplankton
08:15

Visualizing Oceanographic Data to Depict Long-term Changes in Phytoplankton

Published on: July 28, 2023

Area of Science:

  • Paleoclimatology
  • Climate Modeling
  • Geological Science

Background:

  • Global mean annual surface air temperatures are projected to increase by 1.1-6.4°C by 2100.
  • Atmospheric CO2 concentrations are currently higher than in the last 650,000 years and may reach Pliocene levels within 50 years.

Purpose of the Study:

  • To evaluate the reliability of climate models by comparing their Pliocene climate 'retrodictions' with geological records.
  • To determine if past geological records, specifically from the Pliocene, can serve as a reliable guide for understanding future climate change.
  • To assess the accuracy of general circulation models (GCMs) in predicting future climate scenarios.

Main Methods:

  • Analysis of Pliocene geological records.
  • Comparison of GCM climate predictions with paleoclimate data.
  • Evaluation of model 'retrodictions' for past climate conditions.

Main Results:

  • (Results not detailed in the abstract, but the study aims to provide them.)
  • The study will present findings on the accuracy of GCMs in simulating Pliocene warmth and CO2 levels.
  • Insights into the reliability of GCMs for future climate projections will be derived.

Conclusions:

  • The Pliocene geological record offers a valuable analog for understanding future climate change.
  • Assessing GCM performance against Pliocene data is crucial for refining future climate predictions.
  • Uniformitarian principles in geology are tested against modern climate change scenarios.