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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.
Migration00:53

Migration

Migration is long-range, seasonal movement from one region or habitat to another. This common strategy, carried out by many different organisms around the world, is an adaptive response that typically corresponds to changes in an organism’s environment, like resource availability or climate. Migrations can involve huge groups of thousands of animals as well as single individuals traveling alone and can range from thousands of kilometers to just a few hundred meters.
Speciation Rates01:07

Speciation Rates

Overview
Genetic Drift03:33

Genetic Drift

Natural selection—probably the most well-known evolutionary mechanism—increases the prevalence of traits that enhance survival and reproduction. However, evolution does not merely propagate favorable traits, nor does it always benefit populations.
Convergent Evolution01:54

Convergent Evolution

Evolution shapes the features of organisms over time, ensuring that they are suited for the environments in which they live. Sometimes, selection pressure leads to the rise of similar but unrelated adaptations in organisms with no recent common ancestors, a process known as convergent evolution.
Habitat Fragmentation02:31

Habitat Fragmentation

Habitat fragmentation describes the division of a more extensive, continuous habitat into smaller, discontinuous areas. Human activities such as land conversion, as well as slower geological processes leading to changes in the physical environment, are the two leading causes of habitat fragmentation. The fragmentation process typically follows the same steps: perforation, dissection, fragmentation, shrinkage, and attrition.

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Related Experiment Video

Updated: May 9, 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

Tracking Nile Delta vulnerability to Holocene change.

Nick Marriner1, Clément Flaux, Christophe Morhange

  • 1Centre National de la Recherche Scientifique, Laboratoire Chrono-Environnement, Université de Franche-Comté, Besançon, France. marriner@cerege.fr

Plos One
|August 8, 2013
PubMed
Summary

The Nile Delta experienced reduced sediment accretion and increased erosion after 4000 years ago due to climate shifts and human activity. This delta

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Area of Science:

  • Earth Sciences
  • Paleoclimatology
  • Geomorphology

Background:

  • Deltaic resilience is crucial for understanding wetland responses to climate change.
  • Holocene climate shifts and human impacts significantly influence deltaic systems.
  • The Nile Delta serves as a key archive for studying long-term environmental changes.

Purpose of the Study:

  • To reconstruct the Nile Delta's 8000-year mass balance record.
  • To understand the delta's response to past hydrological shifts and climate change.
  • To assess the interplay between climate, human impacts, and deltaic evolution.

Main Methods:

  • Analysis of an 8000-year mass balance record from the Nile Delta.
  • Reconstruction of past hydrological shifts and sediment supply variations.
  • Correlation with global Holocene climate proxies and anthropogenic activity timelines.

Main Results:

  • Nile Delta accretion rates decreased significantly after ~4000 years ago.
  • Sediment loss and erosion intensified following reduced sediment supply and increased human impacts (Pharaonic period).
  • Weakened monsoonal precipitation and reduced river flow facilitated human expansion on the delta.

Conclusions:

  • The Nile Delta exhibits a long history of vulnerability to climate change, sea-level rise, and extreme events.
  • Human activities, particularly from the Pharaonic period, significantly altered deltaic processes.
  • Modern sediment-starved conditions present a novel challenge with no direct Holocene analogue, highlighting the need for deltaic research.