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![Elytron of Plateumaris sp. from middle Pleistocene <span class="search-highlight">Hirabaru</span> <span class="search-highlight">Formation</span>. A:...]()
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Hirabaru Formation
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Image
Elytron of Plateumaris sp. from middle Pleistocene Hirabaru Formation. A:...
Published: 01 February 2010
Figure 3. Elytron of Plateumaris sp. from middle Pleistocene Hirabaru Formation. A: Transmission electron micrograph (TEM) of vertical section of elytron showing laminations of alternating greater and lesser electron density, distinguishing epicuticle (Ep) from exocuticle (Ex). B: TEM image
Journal Article
Original structural color preserved in an ancient leaf beetle
Journal: Geology
Publisher: Geological Society of America
Published: 01 February 2010
Geology (2010) 38 (2): 127–130.
...Figure 3. Elytron of Plateumaris sp. from middle Pleistocene Hirabaru Formation. A: Transmission electron micrograph (TEM) of vertical section of elytron showing laminations of alternating greater and lesser electron density, distinguishing epicuticle (Ep) from exocuticle (Ex). B: TEM image...
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Image
Reflected light micrographs. Same intensity of unidirectional white light w...
Published: 01 February 2010
Figure 2. Reflected light micrographs. Same intensity of unidirectional white light was used for each specimen. A: Plateumaris sp. from middle Pleistocene Hirabaru Formation, Japan. B: Holocene leaf beetle Plateumaris sericea (Japan).
Book Chapter
Triassic
Series: SEPM Concepts in Sedimentology and Paleontology
Publisher: SEPM Society for Sedimentary Geology
Published: 01 January 2013
DOI: 10.2110/sepmcsp.11.156
EISBN: 9781565762893
...-160) discussed Late Triassic coals. The Rijks Geologische Dienst (1982) cited the Carnian and Carnian/Norian Aso, Momonokie and Hirabaru Formations of the Omine Coalfield (C283: 34°N, 131.5°E). ESCAP (1988) cited the Mine Group and the Nariwa Group from southwestern Honshu, including both Carnian...
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