Biodiversity

Biodiversity

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Introduction

caption Reef fishes and corals at French Frigate Shoals, Northwest Hawaiian Islands. Corals reefs are the most diverse marine ecoystems. Photo by James Watt.

The word "biodiversity" is a contracted version of "biological diversity". The Convention on Biological Diversity defines biodiversity as:"the variability among living organisms from all sources including, inter alia, terrestrial, marine and other aquatic ecosystems and the ecological complexes of which they are a part; this includes diversity within species, between species, and of ecosystems." 

Thus, biodiversity includes genetic variation within species, the variety of species in an area, and the variety of habitat types within a landscape. Perhaps inevitably, such an all-encompassing definition, together with the strong emotive power of the concept, has led to somewhat cavalier use of the term biodiversity, in extreme cases to refer to life or biology itself. But biodiversity properly refers to the variety of living organisms.

Biological diversity is of fundamental importance to the functioning of all natural and human-engineered ecosystems, and by extension to the ecosystem services that nature provides free of charge to human society. Living organisms play central roles in the cycles of major elements (carbon, nitrogen, and so on) and water in the environment, and diversity specifically is important in that these cycles require numerous interacting species.

General interest in biodiversity has grown rapidly in recent decades, in parallel with the growing concern about nature conservation generally, largely as a consequence of accelerating rates of natural habitat loss, habitat fragmentation and degradation, and resulting extinctions of species. The IUCN Red List estimates that 12-52% of species within well-studied higher taxa such as vertebrates and vascular plants are threatened with extinction. Based on data on recorded extinctions of known species over the past century, scientists estimate that current rates of species extinction are about 100 times higher than long-term average rates based on fossil data. Other plausuble estimates suggest that present extinction rates now may have reached 1000 to 10,000 times the average over past geologic time. These estimates are the basis of the consensus that the Earth is in the midst of the sixth mass extinction event in its history; the present extinction event is termed the Holocene Mass Extinction.

The Magnitude of Biodiversity

caption An Australian rain forest Creek.

Biodiversity is most frequently quantified as the number of species. Estimates of the number of species currently living on Earth range widely, largely because most living species are microorganisms and tiny invertebrates, but most estimates fall between 5 million and 30 million species. Roughly 1.75 million species have been formally described and given official names. Insects comprise over half of the described species, and three fourths of known faunal species. The number of undescribed species is undoubtedly much higher, however. Particularly in inaccessible environments, and for inconspicuous groups of organisms, collecting expeditions routinely discover many undescribed species. Estimates of the total numbers of species on Earth have been derived variously by extrapolating from the ratios of described to previously unknown species in quantitative samples, from the judgment of experts in particular taxonomic groups, and from patterns in the description of new species through time. For most groups of organisms other than vertebrates, such estimates are little more than educated guesses, explaining the wide range in estimates of global species diversity. Since insects are essentially absent from the sea, the species diversity of the oceans is generally considerably lower than terrestrial ones.

caption Fig 1. ​Biodiversity of plant life across the planet​. Source: Saikat Basu, own work

Species can be grouped on the basis of shared characteristics into hierarchical groups, or taxa, reflecting their shared evolutionary history. At the highest level of classification (or deepest branches in the evolutionary tree of life) organisms are divided into three Domains: 1) the Bacteria, which are microorganisms lacking a cellular nucleus or other membrane-bound organelles; 2) the relatively recently discovered Archaea, microorganisms of primarily extreme environments such as hot springs, which are superficially similar to Bacteria but fundamentally different at biochemical and genetic levels; and 3) the Eukarya, which include all other organisms based on nucleated cells. The Eukarya includes the four "kingdoms", the protists, animals, plants, and fungi. Each of the eukaryotic kingdoms in turn is divided into a number of phyla. At this higher taxonomic level, the oceans are far more diverse than those on land, likely reflecting the marine origins of life on Earth. Nearly half the phyla of animals occur only in the sea (e.g., the sea stars and other echinoderms), whereas only one (the obscure Onychophora, or velvet worms) is restricted to land.

caption Fig 2. Spectrum of biodiversity showcasing higher forms of life such as Birds (A-C); Amphibian (E), and Mammals (F-G) to lower diverse invertebrates such as crabs (Crustacean, Arthropods, D) to lower forms of spectacular life in the form of fungi such as Basidiomycota (H-I) and Zygomycota (J-N). Source: Saikat Basu, own work

Measurement of biodiversity

Distribution of biodiversity

Species diversity varies systematically across the globe with latitude, longitude, and altitude (or its equivalent, depth, in the oceans). The trend toward higher species diversity in the tropics is perhaps the most conspicuous biogeographic pattern in nature, and is sufficiently general to have been considered a "rule". In most marine groups, diversity is maximal in the Indo-West Pacific.

caption Fig 3. Ecosystems representing unique global biodiversity A. Eastern and B. Western Himalayas, India; C. Mangrove forest of the Sunderbans, India; D. Canadian Rockies, Canada; E. Dry tropical woodland forest, Australia; F. Northern Norway; G. Samalayuca dunes, Mexico; and I. Wetlands, Iran. Photo courtesies: A-D: Saikat Basu; E: Steve Douglas; F: Karoline Lans; G. Juan José Fraire; and I. Peiman Zandi

Superimposed on these large-scale global patterns are local hot spots of diversity generated by geographical features, by quirks of geologic history, or by mixing of biotas from different biogeographic provinces. These biodiversity hot spots have become important (and often controversial) foci for conservation efforts.

Ecological controls on biodiversity

A central question in explaining these patterns of diversity is determining the relative importance of long-term evolutionary processes -- the balance between origin and extinction of species -- and local ecological processes of species interactions.

The general similarity among diversity patterns of different taxa with latitude and region suggests that prehistorically these patterns have been controlled primarily by factors operating over large spatial and temporal scales. Ultimately, the number of species in a region is set by a balance between origin through speciation, loss through extinction, and migration of species among regions, all of which operate over long (geologic) time scales.

Conversely, on local spatial scales and over ecological time scales on the order of a few generations of organisms, a wealth of evidence shows that diversity often varies systematically with habitat area, habitat heterogeneity, disturbance, and availability of energy (i.e., productivity) and other resources, notably water in terrestrial ecosystems.

Human disturbance factors

For the most recent 10,000 years man has been the greatest factor affecting biodiversity, with adverse impacts occurring at an accelerating pace since approximately the Industrial Revolution. Human intervention in ecosystem function have been expressed through habitat destruction, habitat fragmentation, overexploitation, and pollution. In some locations such as Easter Island and Hawaii the majority of macroscopic species that existed as recently as the mid-Holocene are now extirpated.

Further reading

  • Bryant, Peter J. 2004. Biodiversity and conservation
  • Gaston, K.J. and J.I. Spicer. 2004. Biodiversity. An introduction. 2nd Edition. Blackwell.ISBN: 1405118571
  • Groombridge, B. and M.D. Jenkins. 2002. World atlas of biodiversity. Earth's living resources in the 21st century. University of California Press, Berkeley.ISBN: 0520236688
  • Hawkins, B.A., Field, R., Cornell, H.V., Currie, D.J., Guegan, J.-F., Kaufman, D.M., Kerr, J.T., Mittelbach, G.G., Oberdorff, T., O'Brien, E.M., Porter, E.E., Turner, JR.G. 2003. Energy, water, and broad-scale geographic patterns of species richness. Ecology 84:3105-3117.
  • Mittelbach, G.G., Steiner, C.F., Scheiner, S.M., Gross, K.L., Reynolds, H.L., Waide, R.B., Willig, M.R., Dodson, S.I., Gough, L. 2001. What is the observed relationship between species richness and productivity? Ecology 82:2381-2396.
  • Purvis, A, and A. Hector. 2000. Getting the measure of biodiversity. Nature 405:212-219.
  • Sala, O.E. et al. 2000. Global Biodiversity Scenarios for the Year 2100. Science 287:1770-1774.
  • Sponsel, Leslie E. Environment in Focus: Sacred places and biodiversity conservation.  Feature includes a timeline, FAQs, supplemental reading, websites, and news stories related to sacred places and biodiversity conservation.
  • UNEP. 2006. Millennium Ecosystem Assessment: Ecosystems and Human-Well Being: Biodiversity Synthesis.ISBN: 1569735883
  • Wilson, E.O. (editor). 1988. Biodiversity, National Academy Press, Washington, DC.ISBN: 0309037395
 
 
Glossary

Citation

(2014). Biodiversity. Retrieved from http://www.eoearth.org/view/article/51cbed137896bb431f68f88b

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