Enigmatic Late Cretaceous high palaeo-latitude lonestones in Chukotka, northeasternmost Asia
(2002) In GFF 124(4). p.197-199- Abstract
- Well-rounded cobbles were encountered within a low-energy restricted marine organic-rich deposit of latest Cretaceous age in Chukotka, NE Asia. The clasts are hydrodynamically incompatible with the inferred quiet depositional environment of the host sediment. Driftwood capable of tree-rafting, glacial striations, gastrolith clast clustering, and disrupting clast impact impressions typical of volcanic ejecta were absent, as were signs of traction currents. If indeed ice-rafting is responsible, this supports recent climate models and palaeobotanical data which favour seasonal marine ice cover of high northern latitudes over a wide span of boundary conditions.
    Please use this url to cite or link to this publication:
    https://lup.lub.lu.se/record/317332
- author
- Ahlberg, Anders LU ; Herman, AB ; Raikevich, M ; Rees, A and Spicer, RA
- organization
- publishing date
- 2002
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Russia, dropstones, lonestones, Cretaceous
- in
- GFF
- volume
- 124
- issue
- 4
- pages
- 197 - 199
- publisher
- Taylor & Francis
- external identifiers
- 
                - wos:000181306200003
- scopus:3843133246
 
- ISSN
- 2000-0863
- DOI
- 10.1080/11035890201244197
- language
- English
- LU publication?
- yes
- id
- 3e4a8302-59bd-41a9-adef-46cb753649d0 (old id 317332)
- date added to LUP
- 2016-04-01 11:58:52
- date last changed
- 2025-10-14 10:48:50
@article{3e4a8302-59bd-41a9-adef-46cb753649d0,
  abstract     = {{Well-rounded cobbles were encountered within a low-energy restricted marine organic-rich deposit of latest Cretaceous age in Chukotka, NE Asia. The clasts are hydrodynamically incompatible with the inferred quiet depositional environment of the host sediment. Driftwood capable of tree-rafting, glacial striations, gastrolith clast clustering, and disrupting clast impact impressions typical of volcanic ejecta were absent, as were signs of traction currents. If indeed ice-rafting is responsible, this supports recent climate models and palaeobotanical data which favour seasonal marine ice cover of high northern latitudes over a wide span of boundary conditions.}},
  author       = {{Ahlberg, Anders and Herman, AB and Raikevich, M and Rees, A and Spicer, RA}},
  issn         = {{2000-0863}},
  keywords     = {{Russia; dropstones; lonestones; Cretaceous}},
  language     = {{eng}},
  number       = {{4}},
  pages        = {{197--199}},
  publisher    = {{Taylor & Francis}},
  series       = {{GFF}},
  title        = {{Enigmatic Late Cretaceous high palaeo-latitude lonestones in Chukotka, northeasternmost Asia}},
  url          = {{http://dx.doi.org/10.1080/11035890201244197}},
  doi          = {{10.1080/11035890201244197}},
  volume       = {{124}},
  year         = {{2002}},
}