2015
DOI: 10.3762/bjnano.6.68
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Mandibular gnathobases of marine planktonic copepods – feeding tools with complex micro- and nanoscale composite architectures

Abstract: SummaryCopepods are dominant members of the marine zooplankton. Their diets often comprise large proportions of diatom taxa whose silicified frustules are mechanically stable and offer protection against grazers. Despite of this protection, many copepod species are able to efficiently break even the most stable frustule types. This ability requires specific feeding tools with mechanically adapted architectures, compositions and properties. When ingesting food, the copepods use the gnathobases of their mandible… Show more

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Cited by 24 publications
(13 citation statements)
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“…Like in the silica-containing teeth of C. hamatus , these resilin-containing structures very likely function as compressible supports reducing the risk of mechanical damages of the teeth during feeding on diatoms with stable frustules. In general, the complex composite systems in the gnathobase teeth are assumed to have co-evolved within an evolutionary arms race together with the diatom frustules [122]. …”
Section: Reviewmentioning
confidence: 99%
“…Like in the silica-containing teeth of C. hamatus , these resilin-containing structures very likely function as compressible supports reducing the risk of mechanical damages of the teeth during feeding on diatoms with stable frustules. In general, the complex composite systems in the gnathobase teeth are assumed to have co-evolved within an evolutionary arms race together with the diatom frustules [122]. …”
Section: Reviewmentioning
confidence: 99%
“…Reports of silicified mandibles have been reported in copepods (Beklemishev, 1954;Miller et al, 1990;Michels et al, 2012;Michels and Gorb, 2015) and amphipods (Mekhanikova et al, 2012). More recently we described silicified teeth in the gastric mill of the blue crab (Vatcher et al, 2015;Nesbit and Roer, 2016).…”
Section: Discussionmentioning
confidence: 99%
“…Geographic distribution: Although benthic foraminifera are common around Antarctica and can be quite diverse (Mikhalevich, 2004), they are often not preserved because the Antarctic shelf waters are highly undersaturated with respect to calcite (Expedition 318 Scientists, 2011), and the remineralization of organic matter causes acidic pore waters which dissolve the foraminifera post-depositional. The inner linings of benthic foraminifera within palynomorph assemblages are found more commonly at sites along the Antarctic coast (Wrenn et al, 1998;Warny et al, 2006;Warny, 2009).…”
Section: Phylum Foraminifera D'orbigny 1826mentioning
confidence: 99%