Phytolith

Image of a phytolith (bulliform)

Phytoliths (from Greek, "plant stone") are rigid, microscopic structures made of silica, found in some plant tissues and persisting after the decay of the plant. These plants take up silica from the soil, whereupon it is deposited within different intracellular and extracellular structures of the plant. Phytoliths come in varying shapes and sizes. Although some use "phytolith" to refer to all mineral secretions by plants, it more commonly refers to siliceous plant remains. In contrast, mineralized calcium secretions in cacti are composed of calcium oxalates.[1]

Functions

There is still debate in the scientific community as to why plants form phytoliths, and whether silica should be considered an essential nutrient for plants. Studies that have grown plants in silica-free environments have typically found that plants lacking silica in the environment do not grow well. For example, the stems of certain plants will collapse when grown in soil lacking silica. In many cases, phytoliths appear to lend structure and support to the plant, much like the spicules in sponges and leather corals. Phytoliths may also provide plants with protection. These rigid silica structures help to make plants more difficult to consume and digest, lending the plant's tissues a grainy or prickly texture.[2] Phytoliths also appear to provide physiologic benefits. Experimental studies have shown that the silicon dioxide in phytoliths may help to alleviate the damaging effects of toxic heavy metals, such as aluminum. Finally, calcium oxalates serve as a reserve of carbon dioxide. Cacti use these as a reserve for photosynthesis during the day when they close their pores to avoid water loss; baobabs use this property to make their trunks more flame-resistant.

History of phytolith research

According to Dolores Piperno, an expert in the field of phytolith analysis, there have been four important stages of phytolith research throughout history.[1][3]

  1. Discovery and exploratory stage (1835–1895): The first report on phytoliths was published by a German botanist named Struve in 1835. During this time another German scientist named Christian Gottfried Ehrenberg was one of the leaders in the field of phytolith analysis. He developed the first classification system for phytoliths, and analyzed soil samples that were sent to him from all around the world. Most notably, Ehrenberg recorded phytoliths in samples he received from the famous naturalist, Charles Darwin, who had collected the dust from the sails of his ship, HMS Beagle, off the coast of the Cape Verde Islands.
  2. Botanical phase of research (1895–1936): Phytolith structures in plants gained wide recognition and attention throughout Europe. Research on production, taxonomy and morphology exploded. Detailed notes and drawings on plant families that produce silica structures and morphology within families were published.
  3. Period of ecological research (1955–1975): First applications of phytolith analysis to paleoecological work, mostly in Australia, the United States, the United Kingdom, and Russia. Classification systems for differentiation within plant families became popular.
  4. Modern period of archaeological and paleoenvironmental research (1978–present): Archaeobotanists working in the Americas first consider and analyze phytolith assemblages in order to track prehistoric plant use and domestication. Also for the first time, phytolith data from pottery are used to track history of clay procurement and pottery manufacture. Around the same time, phytolith data are also used as a means of vegetation reconstruction among paleoecologists. A much larger reference collection on phytolith morphology within varying plant families is assembled.

Development in plants

First, soluble silica, also called monosilicic acid, is taken up from the soil when plant roots absorb groundwater. From there, it is carried to other plant organs by the xylem. By an unknown mechanism, which appears to be linked to genetics and metabolism, some of the silica is then laid down in the plant as silicon dioxide. This biological mechanism does not appear to be limited to specific plant structures, as some plants have been found with silica in their reproductive and sub-surface organs.[1]

Chemical and physical characteristics

Phytoliths are composed mainly of noncrystalline silicon dioxide, and about 4% to 9% of their mass is water. Carbon, nitrogen, and other major nutrient elements comprise less than 5%, and commonly less than 1%, of phytolith material by mass. These elements are present in the living cells in which the silica concretions form, so traces are retained in the phytoliths. Such immobilised elements, in particular carbon, are valuable in that they permit radiometric dating in reconstructing past vegetation patterns. The silica in phytoliths has a refractive index ranging from 1.41 to 1.47, and a specific gravity from 1.5 to 2.3. Phytoliths may be colorless, light brown, or opaque; most are transparent. Phytoliths exist in various three-dimensional shapes, some of which are specific to plant families, genera or species.

Single cell and conjoined phytoliths

Phytoliths may form within single cells, or multiple cells within a plant to form 'conjoined' or multi-cell phytoliths, which are three-dimensional replicas of sections of plant tissue. Conjoined phytoliths occur when conditions are particularly favourable for phytolith formation, such as on a silica rich substrate with high water availability[4]

Patterns of phytolith production

Because identification of phytoliths is based on morphology, it is important to note taxonomical differences in phytolith production.[1]

Families with high phytolith production; family and genus-specific phytolith morphology is common:

Families where phytolith production may not be high; family and genus-specific phytolith morphology is common:

Families where phytolith production is common; family and genus-specific phytolith morphology is uncommon:

Families where phytolith productions varies; family and genus-specific phytolith morphology is uncommon:

Families where phytolith production is rare or not observed:

Archaeology

Phytoliths are very robust, and are useful in archaeology because they can help to reconstruct the plants present at a site when the rest of the plant parts have been burned up or dissolved. Because they are made of the inorganic substances silica or calcium oxalate, phytoliths don't decay with the rest of the plant and can survive in conditions that would destroy organic residues. Phytoliths can provide evidence of both economically important plants and those that are indicative of the environment at a particular time period.

Phytoliths may be extracted from residue on many sources: dental calculus (buildup on teeth); food preparation tools like rocks, grinders, and scrapers; cooking or storage containers; ritual offerings; and garden areas.

Sampling strategies

  1. Cultural contexts: The most important consideration when designing a sampling strategy for a cultural context is to fit the sampling design to the research objectives. For example, if the objective of the study is to identify activity areas, it may be ideal to sample using a grid system. If the objective is to identify foodstuffs, it may be more beneficial to focus on areas where food processing and consumption took place. It is always beneficial to sample ubiquitously throughout the site, because it is always possible to select a smaller portion of the samples for analysis from a larger collection. Samples should be collected and labeled in individual plastic bags. It is not necessary to freeze the samples, or treat them in any special way because silica is not subject to decay by microorganisms.[5]
  2. Natural contexts: Sampling a natural context, typically for the purpose of environmental reconstruction, should be done in a context that is free of disturbances. Human activity can alter the makeup of samples of local vegetation, so sites with evidence of human occupation should be avoided. Bottom deposits of lakes are usually a good context for phytolith samples, because wind often will carry phytoliths from the topsoil and deposit them on water, where they will sink to the bottom, very similar to pollen. It is also possible and desirable to take vertical samples of phytolith data, as it can be a good indicator of changing frequencies of taxa over time.[5]
  3. Modern surfaces: Sampling modern surfaces for use with archeobotanical data may be used to create a reference collection, if the taxa being sampled are known. It may also serve to "detect downward movement of phytoliths into archaeological strata".[5] Taking point samples for modern contexts is ideal.

Laboratory analysis

Elephant grass phytolith processed by dry ashing

The first step in the laboratory analysis of phytolith samples is processing, in order to extract the phytoliths from the soil. Phytoliths can be extracted from soil samples in two ways: chemically or by ashing. After processing, microscopy is used to identify the phytoliths. Optical microscopes with magnifications of 200-400x are typically used to screen phytoliths. Scanning electron microscopy may also allow for a more detailed study of phytoliths.[5]

Contribution to archaeobotanical knowledge

Tracing the history of plant-human interactions

Problems with phytolith analysis of remains

  1. Multiplicity: different parts of a single plant may produce different phytoliths.
  2. Redundancy: different plants can produce the same kind of phytolith.[12]
  3. Some plants produce large numbers of phytoliths while others produce only few.[10]

Taxonomic resolution issues deriving from the multiplicity and redundancy problems can be dealt with by integrating phytolith analysis with other areas, such as micromorphology and morphometric approaches used in soil analysis.[13] It is suggested that using phytolith data from food residues (on ceramics, usually) can decrease the bias from both of these problems, because phytolith analysis is more likely to represent crop products and identification of phytoliths can be made with more confidence. Also, food residues do not usually accumulate extraneous deposits. In other words, the samples are more likely to represent a primary context.[6]

Palaeontology and Paleoenvironmental reconstructions

Phytoliths occur abundantly in the fossil record,[14] and have been reported from the Late Devonian onwards.[14] Robustness of phytoliths make them available to be found in various remains including sedimentary deposits, coprolites, and dental calculus from diverse environmental conditions.[15] In addition to reconstructing human-plant interactions since the Pleistocene, phytoliths can be used to identify palaeoenvironments and to track vegetational change.[14] More and more studies are acknowledging phytolith records as a valuable tool for reconstructing pre-Quaternary vegetation changes (e.g.,[16][17][18][19][20][21][22][23][24]). Occasionally, paleontologists find and identify phytoliths associated with extinct plant-eating animals (i.e. herbivores). Findings such as these reveal useful information about the diet of these extinct animals, and also shed light on the evolutionary history of many different types of plants. Paleontologists in India have recently identified grass phytoliths in dinosaur dung (coprolites), strongly suggesting that the evolution of grasses began earlier than previously thought.[25]

Phytolith records in the context of the global silica cycle, along with CO2 concentrations and other paleoclimatological records, can help constrain estimates of certain long-term terrestrial, biogeochemical cycles and interrelated climate changes.[26]

Light intensity (e.g., open versus closed canopies) can affect cell morphology, especially cell length and area, which can be measured from phytolith fossils. These can be useful for tracing fluctuations in the ancient light regime and canopy cover.[27]

Freshwater oases and related landscape changes that could have affected plant-human interactions were reconstructed through synthesizing phytolith, pollen, and paleoenvironmental data in the well-known early hominin site of Olduvai Gorge in Tanzania.[28]

Comparisons between paleorecords of phytolith remains and modern reference remains in the same region can aid reconstructing how plant composition and related environments changed over time.[10]

Though further testing is required, evolution and development of phytoliths in vascular plants seem to be related to certain types of plant-animal interactions in which phytoliths function as a defensive mechanism for herbivores or related to adaptive changes to habitats.[29]

Japanese and Korean archaeologists refer to grass and crop plant phytoliths as "plant opal" in archaeological literature.

For extended examples of phytolith taxonomy, see the University of Sheffield's comprehensive Phytolith Interpretation page.

Carbon sequestration

Research, particularly since 2005 has shown that carbon in phytoliths can be resistant to decomposition for millennia and can accumulate in soils.[30] While researchers had previously known that phytoliths could persist in some soils for thousands of years [31] and that there was carbon occluded within phytoliths that could be used for radiocarbon dating,[32] research into the capacity of phytoliths as a method of storing carbon in soils was pioneered by Parr and Sullivan [33] suggested that there was a real opportunity to sequester carbon securely in soils for the long term, in the form of carbon inclusions in durable silica phytoliths. Subsequent research has shown the effectiveness of phytoliths as a process to sequester carbon using a range of agricultural crops and other economically important plants. While carbon sequestration is a potentially important way to limit atmospheric greenhouse gas concentrations in the long term, the use of phytoliths to achieve this must be balanced against other uses that might be made of the same biomass carbon (or land for producing biomass) to reduce GHG emissions by other means including, for example, the production of bioenergy to offset fossil fuel emissions. If enhanced phytolith production results in a reduced availability of biomass for other GHG mitigation strategies, its effectiveness for lowering net GHG emissions may be reduced or negated.

See also

References

  1. 1 2 3 4 Piperno, Dolores R. (2006). Phytoliths: A Comprehensive Guide for Archaeologists and Paleoecologists. AltaMira Press ISBN 0759103852.
  2. ↑ Hunt, JW; Dean, AP; Webster, RE; Johnson, GN; Ennos, AR (2008). "A novel mechanism by which silica defends grasses against herbivory". Ann Bot. 102 (4): 653–6. PMC 2701777 Freely accessible. PMID 18697757. doi:10.1093/aob/mcn130.
  3. ↑ Phytoliths Gallery. Smithsonian National Museum of Natural History.
  4. ↑ Jenkins, Emma (2009). "Phytolith taphonomy: a comparison of dry ashing and acid extraction on the breakdown of conjoined phytoliths formed in Triticum durum". Journal of Archaeological Science. 36: 2402–2407. doi:10.1016/j.jas.2009.06.028.
  5. 1 2 3 4 Pearsall, Deborah. (2000). Paleoethnobotany: a Handbook of Procedures. Academic Press: San Diego ISBN 0125480423.
  6. 1 2 Lustek, Robert Karl. (2008). Setting the Archaeology of Maize on Its Ear: The Use of Phytolith Assemblages to Identify Lineages of Maize. University of Minnesota ISBN 0549717765.
  7. ↑ Harvey, Emma L.; Fuller, Dorian Q (2005). "Investigating crop processing using phytolith analysis: the example of rice and millets" (PDF). Journal of Archaeological Science. 32 (5): 739–752. JSTOR 5647. doi:10.1016/j.jas.2004.12.010.
  8. ↑ Kealhofer, L (2003). "Looking into the gap: land use and the tropical forests of southern Thailand". Asian Perspectives. 42 (1).
  9. ↑ Kealhofer, L (2002). "Changing perceptions of risk: The development of agro-ecosystems in Southeast Asia". American Anthropologist. 104 (1).
  10. 1 2 3 Tsartsidou, Georgia; Lev-Yadun, Simcha; Albert, Rosa-Maria; Miller-Rosen, Arlene; Efstratiou, Nikos; Weiner, Steve (2007). "The phytolith archaeological record: strengths and weaknesses evaluated based on a quantitative modern reference collection from Greece". Journal of Archaeological Science. 34 (8): 1262–1275. ISSN 0305-4403. doi:10.1016/j.jas.2006.10.017.
  11. ↑ Piperno, D. R. (2003). "Phytolith Evidence for Early Holocene Cucurbita Domestication in Southwest Ecuador". Science. 299 (5609): 1054–1057. ISSN 0036-8075. doi:10.1126/science.1080365.
  12. ↑ Shillito, L-M. (2013). "Grains of truth or transparent blindfolds? A review of current debates in archaeological phytolith analysis". Vegetation History and Archaeobotany. 22 (1): 71–82. doi:10.1007/s00334-011-0341-z.
  13. ↑ Hart, Thomas C. (2016). "Issues and directions in phytolith analysis". Journal of Archaeological Science. 68: 24–31. ISSN 0305-4403. doi:10.1016/j.jas.2016.03.001.
  14. 1 2 3 Carter, J.A. (1999). "Late Devonian, Permian and Triassic phytoliths from Antarctica". Micropaleontology. 45 (1): 56–61. JSTOR 1486202. doi:10.2307/1486202.
  15. ↑ Carter, John A (2002). "Phytolith analysis and paleoenvironmental reconstruction from Lake Poukawa Core, Hawkes Bay, New Zealand". Global and Planetary Change. 33 (3–4): 257–267. ISSN 0921-8181. doi:10.1016/S0921-8181(02)00081-4.
  16. ↑ Pinilla, A., and Bustillo, A., 1997, Sílicofi tolitos en secencies arcillosas con silcretas. Mioceno Medio, Madrid,in Pinilla, A., Juan-Tresserras, J., and Machado, M.J., eds., The State of the Art of Phytoliths in Soils and Plants, Volume 4: Madrid, Consejo Superior de Investigaciones Científi cas (CSIC), p. 255–265.
  17. ↑ Strömberg, Caroline A.E (2002). "The origin and spread of grass-dominated ecosystems in the late Tertiary of North America: preliminary results concerning the evolution of hypsodonty". Palaeogeography, Palaeoclimatology, Palaeoecology. 177 (1–2): 59–75. ISSN 0031-0182. doi:10.1016/S0031-0182(01)00352-2.
  18. ↑ Stromberg, C (2004). "Using phytolith assemblages to reconstruct the origin and spread of grass-dominated habitats in the great plains of North America during the late Eocene to early Miocene". Palaeogeography, Palaeoclimatology, Palaeoecology. 207 (3–4): 239–275. ISSN 0031-0182. doi:10.1016/j.palaeo.2003.09.028.
  19. ↑ Strömberg, C.A.E., Friis, E.M., Liang, M.-M., Werdelin, L.,and Zhang, Y.-l., 2007a, Palaeoecology of an early middle Miocene lake in China: Preliminary interpretations based on phytoliths from the Shanwang Basin:Vertebrata PalAsiatica, v. 45, no. 2, p. 145–160.
  20. ↑ Strömberg, Caroline A.E.; Werdelin, Lars; Friis, Else Marie; Saraç, Gerçek (2007). "The spread of grass-dominated habitats in Turkey and surrounding areas during the Cenozoic: Phytolith evidence". Palaeogeography, Palaeoclimatology, Palaeoecology. 250 (1–4): 18–49. ISSN 0031-0182. doi:10.1016/j.palaeo.2007.02.012.
  21. ↑ WoldeGabriel, G.; Ambrose, S. H.; Barboni, D.; Bonnefille, R.; Bremond, L.; Currie, B.; DeGusta, D.; Hart, W. K.; Murray, A. M.; Renne, P. R.; Jolly-Saad, M. C.; Stewart, K. M.; White, T. D. (2009). "The Geological, Isotopic, Botanical, Invertebrate, and Lower Vertebrate Surroundings of Ardipithecus ramidus". Science. 326 (5949): 65–65, 65e1–65e5. ISSN 0036-8075. doi:10.1126/science.1175817.
  22. ↑ Zucol, A.F., Brea, M., and Bellosi, E., 2010, Phytolith studies in Gran Barranca (central Patagonia, Argentina): The middle-late Eocene, in Madden, R.H., Carlini, A.A.,Vucetich, M.G., and Kay, R.F., eds., The Paleontology of Gran Barranca: Evolution and Environmental Change through the Middle Cenozoic of Patagonia: Cambridge, UK, Cambridge University Press, p. 317–340.
  23. ↑ Strömberg, Caroline A. E.; McInerney, Francesca A. (2016). "The Neogene transition from C3 to C4 grasslands in North America: assemblage analysis of fossil phytoliths". Paleobiology. 37 (01): 50–71. ISSN 0094-8373. doi:10.1666/09067.1.
  24. ↑ Miller, L. A.; Smith, S. Y.; Sheldon, N. D.; Stromberg, C. A. E. (2012). "Eocene vegetation and ecosystem fluctuations inferred from a high-resolution phytolith record". Geological Society of America Bulletin. 124 (9–10): 1577–1589. ISSN 0016-7606. doi:10.1130/B30548.1.
  25. ↑ Hecht, Jeff, Fossil dung reveals dinosaurs did graze grass, New Scientist Magazine , 17 November 2005. Accessed January 2008
  26. ↑ Conley, Daniel J. (2002). "Terrestrial ecosystems and the global biogeochemical silica cycle". Global Biogeochemical Cycles. 16 (4): 68–1–68–8. Bibcode:2002GBioC..16.1121C. ISSN 0886-6236. doi:10.1029/2002GB001894.
  27. ↑ Dunn, Regan E.; Le, Thien-Y. T.; Strömberg, Caroline A. E. (2015). "Light Environment and Epidermal Cell Morphology in Grasses". International Journal of Plant Sciences. 176 (9): 832–847. ISSN 1058-5893. doi:10.1086/683278.
  28. ↑ Ashley, Gail M.; Barboni, Doris; Dominguez-Rodrigo, Manuel; Bunn, Henry T.; Mabulla, Audax Z.P.; Diez-Martin, Fernando; Barba, Rebeca; Baquedano, Enrique (2017). "Paleoenvironmental and paleoecological reconstruction of a freshwater oasis in savannah grassland at FLK North, Olduvai Gorge, Tanzania". Quaternary Research. 74 (03): 333–343. ISSN 0033-5894. doi:10.1016/j.yqres.2010.08.006.
  29. ↑ Strömberg, Caroline A. E.; Di Stilio, Verónica S.; Song, Zhaoliang; De Gabriel, Jane (2016). "Functions of phytoliths in vascular plants: an evolutionary perspective". Functional Ecology. 30 (8): 1286–1297. ISSN 0269-8463. doi:10.1111/1365-2435.12692.
  30. ↑ Parr, J; Sullivan, L (2005). "Soil carbon sequestration in phytoliths". Soil Biology and Biochemistry. 37: 117–124. doi:10.1016/j.soilbio.2004.06.013.
  31. ↑ Piperno, D.R.; Hans-Dieter, S. (2005). "Dinosaurs Dined on Grass". Science. 310: 1126–1128. PMID 16293745. doi:10.1126/science.1121020.
  32. ↑ Wilding, L.P. (1967). "Radiocarbon dating of biogenetic opal". Science. 156: 66–67. doi:10.1126/science.156.3771.66.
  33. ↑ Parr, J. F.; Sullivan, L. A. (2005). "Soil carbon sequestration in Phytoliths". Soil Biology and Biochemistry. 37 (1): 117–124. doi:10.1016/j.soilbio.2004.06.013.

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