Research Article| February 01, 2010 Original structural color preserved in an ancient leaf beetle Gengo Tanaka; Gengo Tanaka * 1Gunma Museum of Natural History, 1674-1, Kamikuroiwa, Tomioka, Gunma 370-2345, Japan *E-mail: tanaka@gmnh.pref.gunma.jp. Search for other works by this author on: GSW Google Scholar Hideki Taniguchi; Hideki Taniguchi 2Oita Industrial Research Institute, 4361-10, Takae-nishi 1, Oita 870-1117, Japan Search for other works by this author on: GSW Google Scholar Haruyoshi Maeda; Haruyoshi Maeda 3Department of Geology and Mineralogy, Kyoto University, Kitashirakawa Oiwakecho Sakyo-ku, Kyoto 606-8502, Japan Search for other works by this author on: GSW Google Scholar Shin-ichi Nomura Shin-ichi Nomura 3Department of Geology and Mineralogy, Kyoto University, Kitashirakawa Oiwakecho Sakyo-ku, Kyoto 606-8502, Japan Search for other works by this author on: GSW Google Scholar Author and Article Information Gengo Tanaka * 1Gunma Museum of Natural History, 1674-1, Kamikuroiwa, Tomioka, Gunma 370-2345, Japan Hideki Taniguchi 2Oita Industrial Research Institute, 4361-10, Takae-nishi 1, Oita 870-1117, Japan Haruyoshi Maeda 3Department of Geology and Mineralogy, Kyoto University, Kitashirakawa Oiwakecho Sakyo-ku, Kyoto 606-8502, Japan Shin-ichi Nomura 3Department of Geology and Mineralogy, Kyoto University, Kitashirakawa Oiwakecho Sakyo-ku, Kyoto 606-8502, Japan *E-mail: tanaka@gmnh.pref.gunma.jp. Publisher: Geological Society of America Received: 14 Jul 2009 Revision Received: 01 Aug 2009 Accepted: 28 Aug 2009 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2010 Geological Society of America Geology (2010) 38 (2): 127–130. https://doi.org/10.1130/G25353.1 Article history Received: 14 Jul 2009 Revision Received: 01 Aug 2009 Accepted: 28 Aug 2009 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Gengo Tanaka, Hideki Taniguchi, Haruyoshi Maeda, Shin-ichi Nomura; Original structural color preserved in an ancient leaf beetle. Geology 2010;; 38 (2): 127–130. doi: https://doi.org/10.1130/G25353.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Greenish-blue metallic colored fossil elytra of the leaf beetle (Plateumaris sp.) have been discovered in the peat sediment of the middle Pleistocene (ca. 600 ka) Hirabaru Formation, Kyushu, Japan. Scanning and transmission electron microscopy revealed the smooth outer surface of the fossil elytra and five alternating electron-dense and electron-lucent layers in the epicuticle. By applying the matrix method to the epicuticle, three reflective peaks of wavelengths 388 nm, 544 nm, and 656 nm were computed. These peaks correspond to the reflective color observed under white light. Thus, the coloration of the fossils was caused by multilayer reflectors of the epicuticle of the elytra. Pyrolysis–gas chromatography–mass spectrometric analysis revealed that the fossil elytra have preserved some of their original macromolecules (chitin, protein, and amino acids), which are similar to those of a related Holocene species. The high-porosity matrix of the peat contains many fragments of diatoms, indicating the high productivity of the water column but a reducing bottom environment. Slight acidity of the interstitial water also seems to contribute to the preservation of some original macromolecules of fossil insects through geologic time. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Read more