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Related Concept Videos

The Fossil Record02:56

The Fossil Record

The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
What is Evolutionary History?02:35

What is Evolutionary History?

Scientists record evolutionary history by analyzing fossil, morphological, and genetic data. The fossil record documents the history of life on Earth and provides evidence for evolution. However, both fossil and living organisms offer evidence that outlines Earth’s evolutionary history.
Conservation of Declining Populations02:07

Conservation of Declining Populations

Conservation of declining population focuses on ways of detecting, diagnosing, and halting a population decline. The approach uses methods to prevent populations from going extinct.
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.
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.
The Tree of Life - Bacteria, Archaea, Eukaryotes02:40

The Tree of Life - Bacteria, Archaea, Eukaryotes

The “tree of life” describes the evolution of life and the evolutionary relationships between organisms. The root of the tree is the common ancestor to all life on Earth. All other species radiate from this point, much like the branches of a tree. The numerous tips of these branches on the tree of life represent every living, or extant, species. Extinct species, which are species that no longer exist, can be found towards the center of the tree. Currently, these organisms, both extant and...

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Related Experiment Video

Updated: May 28, 2026

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

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A warrant for applied palaeozoology.

R Lee Lyman1

  • 1Department of Anthropology, 107 Swallow Hall, University of Missouri, Columbia, MO 65211, USA. lymanr@missouri.edu

Biological Reviews of the Cambridge Philosophical Society
|October 29, 2011
PubMed
Summary

The fossil record, or palaeozoological record, is valuable for conservation biology. It provides crucial historical data on biological change, similar to natural history collections, aiding modern resource management.

Area of Science:

  • Paleozoology
  • Conservation Biology
  • Neozoology

Background:

  • Debate exists on the utility of the palaeozoological record for conservation biology due to perceived biases.
  • Natural history collections (NHCs) offer valuable historical data for understanding biological change.
  • Many variables documented in NHCs are also identifiable in the palaeozoological record.

Purpose of the Study:

  • To evaluate the value of the palaeozoological record for conservation biology.
  • To address the argument that the palaeozoological record is too incomplete for conservation purposes.
  • To demonstrate the utility of palaeozoological data in modern resource management.

Main Methods:

  • Comparative analysis of data from natural history collections and palaeozoological remains.

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  • Identification of variables documenting global biological change across different time scales.
  • Review of empirical examples using palaeozoological data in conservation contexts.
  • Main Results:

    • The palaeozoological record contains variables crucial for conservation biology, mirroring data from NHCs.
    • These variables provide significant time depth, essential for documenting global biological change.
    • Empirical evidence supports the use of palaeozoological data for conservation and resource management.

    Conclusions:

    • The palaeozoological record is a valuable and satisfactory resource for conservation biology.
    • Palaeozoological data should be consulted for modern resource management and understanding biological change.
    • The historical perspective offered by the fossil record complements data from contemporary collections.