Calcareous nannofossils

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"Nannoplankton" redirects here. For the generic diminutive plankton, see Plankton § Size groups, and Nanophytoplankton.
Quaternary period

Calcareous nannofossils are a class of tiny (less than 30

single-cell organisms forming them (nannoplankton)[3] and ease of handling of the sediment samples.[4] The practical applications of calcareous nannofossils in the areas of biostratigraphy and paleoecology[5] became clear once the deepwater drilling took off in 1968 with the Deep Sea Drilling Project,[4] and they have been extensively studied ever since.[5] Nannofossils provide one of the most important paleontological records with the contiguous length of 220 million years.[6]

History of research

Part of a series related to
Biomineralization
General
Exoskeletons (shells)
Endoskeletons (bones)
Teeth, scales, tusks etc
Calcification
Silicification
Other forms
Related

coccospheres. Huxley then changed his views and declared that coccoliths are skeletal elements of an unknown organism, Bathybius haeckelii, a primordial form of organic life. One of the goals of the Challenger expedition was to understand the nature of the Bathybius,[7] but the scientists aboard the ship reached the conclusion that the gel-like substance apparently holding the disks in a coccosphere together was a result of processing the samples[7] and later declared the coccoliths to constitute the defensive armor of tiny nannoplankton algae (the term was coined in 1909 by Hans Lohmann [de] to identify the tiniest plankton, less than 60 microns in size, that passed through the regular phytoplankton nets).[4]

Research of the nannoplankton

drilling core was hauled aboard the ship. At the same time, the continuous DSDP cores provided a solid foundation for setting up the nannofossil biozones.[4] It took decades to establish comprehensive chronological schemes (e.g. Martini 1971; Sissingh 1977; Roth 1978; Okada & Bukry 1980).[10]

The researchers started to use the

transmission electron microscopes in the mid-1950s, switching to scanning electron microscopes in the 1960s and 1970s. Optical microscopes with cross-polarization and phase-contrast illumination, techniques introduced in 1952 by Kamptner and Braarud & Nordli respectively, are still used for routine field work.[9]

Terminology

The terminology in the field evolved over time and nannofossils are also sometimes called "nannoplankton" and "coccoliths" as well as some other names, especially in the literature published in 1950s and 1960s. The term "calcareous nannofossil" was chosen in the DSDP publications (although it was rarely used prior to that) and gained popularity afterwards, in the early 1970s.

Latin: calx, "lime", and means "containing lime".[11]

Siesser & Haq describe the general use as follows:[12]

  • coccolith is restricted by some authors to designate round-shaped elements similar to the ones produced by the living coccolithophores. For differently-shaped objects (e. g., stars and horseshoes), nanolith is being used. Some other authors, however, use coccolith in a broader sense for all calcareous nanofossils;
  • nannoplankton is sometimes used to identify the living organisms, with nannofossils referring to the now-extinct species. Other researchers use the nannoplankton for all forms, both living and extinct arguing that even though the true taxonomy of the extinct ones might never be known, their planktic way of living is subject to little doubt.

Siesser & Haq themselves use nannoplankton as a generic way to refer to all organisms, whether living or extinct and nannofossils when describing specifically the fossil forms.

Biostratigraphy

Multiple characteristics of the calcareous nannofossils make them a valuable tool of biostratigraphy and biochronology:[13]

  • continuous record from 220 million years ago to present;
  • abundance in marine sediments;
  • worldwide distribution due to the planktonic nature;
  • rapid evolution (with diverse morphology[14]) that provides hundreds of points of appearance and extinction;
  • tiny size allows the work to be performed with small samples (less than 1 gramm[14]).

The calcareous nannofossils can be found in the deposits that stretch from the Late Triassic to the modern times. The calcareous nannoplankton biodiversity grew in the Jurassic and Cretaceous periods peaking at about 150 species in the Late Cretaceous.[15]

The boundaries of the biozones in stratigraphy are defined by the biohorizons, points in strata where significant changes in fossil content and distribution occur. Typical events used for biohorizons are: first occurrence, last occurrence, change in abundance of taxons. A combination of biozones arranged in stratigraphical order results in a zonation (or scheme).[10]

The first

Palaeocene, CNE for Eocene, CNO for Oligocene, CNM for Miocene, CNPL for Pliocene/Pleistocene (CN stands for Calcareous Nannofossils).[16]

The agreed upon stratification reference is codified as Global Boundary Stratotype Section and Point (GSSP) by the International Commission on Stratigraphy. The calcareous nannofossils, with very few exceptions, provide clear biohorizons indicating the positions of the GSSP boundaries in Cenozoic.[16]

Other uses

Calcareous nannofossils are being used in

tesserae, grounds of paintings, statues, and masonry.[17]

References

  1. ^ Romein 1979, p. 7.
  2. ^ Incarbona et al. 2010, p. 820.
  3. ^ Siesser & Haq 1987, p. 116.
  4. ^ a b c d e Siesser & Haq 1987, p. 90.
  5. ^ a b c Siesser & Haq 1987, p. 87.
  6. ^ Agnini, Monechi & Raffi 2017, p. 449.
  7. ^ a b Siesser & Haq 1987, p. 88.
  8. ^ Siesser 2006, p. 8.
  9. ^ a b Siesser 2006, p. 10.
  10. ^ a b Agnini, Monechi & Raffi 2017, p. 452.
  11. ^ Guilford 1908, p. 822.
  12. ^ Siesser & Haq 1987, p. 92.
  13. ^ Agnini, Monechi & Raffi 2017, pp. 448–449.
  14. ^ a b Falkenberg, Mutterlose & Kaplan 2020, p. 22.
  15. ^ Falkenberg, Mutterlose & Kaplan 2020, p. 19.
  16. ^ a b Agnini, Monechi & Raffi 2017, p. 453.
  17. ^ Falkenberg, Mutterlose & Kaplan 2020, pp. 19–20.

Sources

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