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Related Concept Videos

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.
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.
Threats to Biodiversity01:50

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Related Experiment Video

Updated: May 14, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

Climate change patterns in Amazonia and biodiversity.

Hai Cheng1, Ashish Sinha, Francisco W Cruz

  • 1Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China. cheng021@umn.edu

Nature Communications
|January 31, 2013
PubMed
Summary
This summary is machine-generated.

Amazonia's hydroclimate has varied, impacting biodiversity. Stable western Amazonia climate supports biodiversity, while eastern Amazonia experienced drying, potentially reducing forest resilience.

Related Experiment Videos

Last Updated: May 14, 2026

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

Area of Science:

  • Paleoclimatology
  • Amazonian climate dynamics
  • Biodiversity science

Background:

  • Understanding hydroclimate variability in Amazonia is key to linking climate change and biodiversity.
  • Previous research highlighted the need for detailed regional climate data.

Purpose of the Study:

  • To reconstruct and analyze hydroclimate variations in western and eastern Amazonia over long timescales.
  • To investigate the relationship between past hydroclimate changes and Amazonian biodiversity patterns.

Main Methods:

  • Utilized absolute-dated speleothem oxygen isotope records.
  • Analyzed data from western Amazonia (past 250,000 years) and eastern Amazonia (past 20,000 years).

Main Results:

  • Demonstrated coherent millennial-scale precipitation variability across tropical-subtropical South America.
  • Revealed a quasi-dipole pattern in orbital-scale precipitation variability between western and eastern Amazonia.
  • Indicated modest precipitation increase in western Amazonia and significant drying in eastern Amazonia during the last glacial period.

Conclusions:

  • Higher biodiversity in western Amazonia may be linked to stable climatic conditions, challenging the 'Refugia Hypothesis'.
  • Eastern Amazonia's biodiversity may have been negatively impacted by glacial-interglacial hydroclimate fluctuations and forest fragmentation.