Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite

Analysis of three amber (resinite) samples collected from Middle and Upper Cretaceous sediments in the Taimyr Peninsula, Siberia, indicates that these materials are based on copolymers of biformene (I) and communol (II). No resinites of similar structural character have previously been described and...

Full description

Bibliographic Details
Main Author: Anderson, K.B.
Language:unknown
Published: 2008
Subjects:
58 GEOSCIENCES
AMBER
STRUCTURAL CHEMICAL ANALYSIS
SIBERIA
CRETACEOUS PERIOD
Taimyr
Siberia
Online Access:http://www.osti.gov/servlets/purl/10175238
https://www.osti.gov/biblio/10175238
https://doi.org/10.2172/10175238
id ftosti:oai:osti.gov:10175238
record_format openpolar
spelling ftosti:oai:osti.gov:10175238 2023-07-30T04:07:13+02:00 Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite Anderson, K.B. 2008-02-12 application/pdf http://www.osti.gov/servlets/purl/10175238 https://www.osti.gov/biblio/10175238 https://doi.org/10.2172/10175238 unknown http://www.osti.gov/servlets/purl/10175238 https://www.osti.gov/biblio/10175238 https://doi.org/10.2172/10175238 doi:10.2172/10175238 58 GEOSCIENCES AMBER STRUCTURAL CHEMICAL ANALYSIS SIBERIA CRETACEOUS PERIOD 2008 ftosti https://doi.org/10.2172/10175238 2023-07-11T11:00:59Z Analysis of three amber (resinite) samples collected from Middle and Upper Cretaceous sediments in the Taimyr Peninsula, Siberia, indicates that these materials are based on copolymers of biformene (I) and communol (II). No resinites of similar structural character have previously been described and hence, these samples represent a previously unknown structural sub-class of resinite. Other/Unknown Material Taimyr Siberia SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 58 GEOSCIENCES
AMBER
STRUCTURAL CHEMICAL ANALYSIS
SIBERIA
CRETACEOUS PERIOD
spellingShingle 58 GEOSCIENCES
AMBER
STRUCTURAL CHEMICAL ANALYSIS
SIBERIA
CRETACEOUS PERIOD
Anderson, K.B.
Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
topic_facet 58 GEOSCIENCES
AMBER
STRUCTURAL CHEMICAL ANALYSIS
SIBERIA
CRETACEOUS PERIOD
description Analysis of three amber (resinite) samples collected from Middle and Upper Cretaceous sediments in the Taimyr Peninsula, Siberia, indicates that these materials are based on copolymers of biformene (I) and communol (II). No resinites of similar structural character have previously been described and hence, these samples represent a previously unknown structural sub-class of resinite.
author Anderson, K.B.
author_facet Anderson, K.B.
author_sort Anderson, K.B.
title Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
title_short Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
title_full Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
title_fullStr Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
title_full_unstemmed Middle and upper cretaceous amber from the Taimyr Peninsula, Siberia: Evidence for a new structural sub-class of resinite
title_sort middle and upper cretaceous amber from the taimyr peninsula, siberia: evidence for a new structural sub-class of resinite
publishDate 2008
url http://www.osti.gov/servlets/purl/10175238
https://www.osti.gov/biblio/10175238
https://doi.org/10.2172/10175238
genre Taimyr
Siberia
genre_facet Taimyr
Siberia
op_relation http://www.osti.gov/servlets/purl/10175238
https://www.osti.gov/biblio/10175238
https://doi.org/10.2172/10175238
doi:10.2172/10175238
op_doi https://doi.org/10.2172/10175238
_version_ 1772820396356141056

Similar Items