Selective concentration of iron, titanium, and zirconium substrate minerals within Gregory's diverticulum, an organ unique to derived sand dollars (Echinoidea: Scutelliformes)

被引:0
|
作者
Zachos, Louis G. [1 ]
Ziegler, Alexander [2 ]
机构
[1] Univ Mississippi, Dept Geol & Geol Engn, Oxford, MS 38677 USA
[2] Rhein Friedrich Wilhelms Univ, Bonner Inst Organism Biol, Bonn, Germany
来源
PEERJ | 2024年 / 12卷
基金
美国国家科学基金会;
关键词
Gregory's diverticulum; Heavy minerals; Echinoidea; Mineralogy; Sand dollar; Scutelliformes; Phylogeography; Digestive tract; Behavior; Weight belt; BENTHIC FORAMINIFER; MELLITA-TENUIS; SEDIMENT; GENUS; ECHINODERMATA; PHYLOGENY; CLYPEASTEROIDA; BIOGEOGRAPHY; SYSTEMATICS; PREFERENCE;
D O I
10.7717/peerj.17178
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Gregory's diverticulum, a digestive tract structure unique to a derived group of sand dollars (Echinoidea: Scutelliformes), is filled with sand grains obtained from the substrate the animals inhabit. The simple methods of shining a bright light through a specimen or testing response to a magnet can reveal the presence of a mineral -filled diverticulum. Heavy minerals with a specific gravity of >2.9 g/cm(3) are selectively concentrated inside the organ, usually at concentrations one order of magnitude, or more, greater than found in the substrate. Analyses of diverticulum content for thirteen species from nine genera, using optical mineralogy, powder X-ray diffraction, scanning electron microscopy and energy dispersive X-ray spectroscopy, as well as micro -computed tomography shows the preference for selection of five major heavy minerals: magnetite (Fe3O4), hematite (Fe2O3), ilmenite (FeTiO3), rutile (TiO2), and zircon (ZrSiO4). Minor amounts of heavy or marginally heavy amphibole, pyroxene and garnet mineral grains may also be incorporated. In general, the animals exhibit a preference for mineral grains with a specific gravity of >4.0 g/cm(3), although the choice is opportunistic and the actual mix of mineral species depends on the mineral composition of the substrate. The animals also select for grain size, with mineral grains generally in the range of 50 to 150 mu m, and do not appear to alter this preference during ontogeny. A comparison of analytical methods demonstrates that X-ray attenuation measured using micro -computed tomography is a reliable non-destructive method for heavy mineral quantification when supported by associated analyses of mineral grains extracted destructively from specimens or from substrate collected together with the specimens. Commonalities in the electro-chemical surface properties of the ingested minerals suggest that such characteristics play an important role in the selection process.
引用
收藏
页数:27
相关论文
empty
未找到相关数据