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Related Concept Videos

Threats to Biodiversity01:50

Threats to Biodiversity

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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
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Small population sizes put a species at extreme risk of extinction due to a lack of variation, and a consequent decrease in adaptability. This weakens the chances of survival under pressures such as climate change, competition from other species, or new diseases. Large populations are more likely to survive pressures such as these, as such populations are more likely to harbor individuals that have genetic variants that are adaptive under new stresses. Small populations are much less...
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In a population that is not at Hardy-Weinberg equilibrium, the frequency of alleles changes over time. Therefore, any deviations from the five conditions of Hardy-Weinberg equilibrium can alter the genetic variation of a given population. Conditions that change the genetic variability of a population include mutations, natural selection, non-random mating, gene flow, and genetic drift (small population size).
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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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Gene flow is the transfer of genes among populations, resulting from either the dispersal of gametes or from the migration of individuals.
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Related Experiment Video

Updated: May 24, 2025

JenaTron - An Experimental Approach to Study the Effects of Plant History and Soil History on Grassland Ecosystem Functioning
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Shifting, expanding, or contracting? Range movement consequences for biodiversity.

Jedediah F Brodie1, Benjamin G Freeman2, Philip D Mannion3

  • 1Division of Biological Sciences and Wildlife Biology Program, University of Montana, Missoula, MT 59812, USA; Institute for Biodiversity and Environmental Conservation, Universiti Malaysia Sarawak, 94300 Kota Samarahan, Sarawak, Malaysia.

Trends in Ecology & Evolution
|March 1, 2025
PubMed
Summary
This summary is machine-generated.

Climate change alters species ranges, impacting biodiversity. Understanding these shifts and expansions is crucial for predicting future ecological changes and conserving species globally.

Keywords:
climate changecommunity diversityextinction risklatitudinal diversity gradientpaleoclimaterange shift

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Area of Science:

  • Ecology
  • Biodiversity Science
  • Climate Change Biology

Background:

  • Climate change drives significant alterations in species distribution patterns globally.
  • Observed range shifts and expansions have complex and often overlooked effects on local and global biodiversity.
  • Past climate changes demonstrate that species range dynamics are a key factor in biodiversity responses.

Purpose of the Study:

  • To analyze the divergent consequences of species range shifts and expansions on biodiversity.
  • To provide a framework for understanding how changing species ranges will reshape Earth's biodiversity.
  • To propose key research directions for predicting biodiversity responses to climate change.

Main Methods:

  • Reviewing current understanding of species range dynamics under climate change.
  • Analyzing the predicted impacts of range shifts and expansions on local and global diversity patterns.
  • Synthesizing insights from paleontology and ecological monitoring.

Main Results:

  • Widespread range shifts are expected to increase local diversity in many regions but decrease it in tropical lowlands.
  • Expansions are predicted to maintain diversity at low latitudes and increase it elsewhere, potentially stabilizing global biodiversity.
  • Both shifts and expansions are common, historically significant responses to climate change.

Conclusions:

  • Future biodiversity will be significantly reshaped by climate-driven range dynamics.
  • Further research is needed to leverage paleontological data for long-term insights.
  • Improved monitoring of range limits and incorporation of dispersal barriers are essential for accurate predictions.