Articles | Volume 13, issue 2
https://doi.org/10.5194/essd-13-343-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-13-343-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Database of global glendonite and ikaite records throughout the Phanerozoic
Geological Institute of RAS, Moscow 119017, Russia
Victoria Ershova
Geological Institute of RAS, Moscow 119017, Russia
Institute of Earth Sciences, St. Petersburg State University, 199034
St. Petersburg, Russia
Oleg Vereshchagin
Institute of Earth Sciences, St. Petersburg State University, 199034
St. Petersburg, Russia
Kseniia Vasileva
Institute of Earth Sciences, St. Petersburg State University, 199034
St. Petersburg, Russia
Kseniia Mikhailova
Institute of Earth Sciences, St. Petersburg State University, 199034
St. Petersburg, Russia
Aleksei Krylov
Institute of Earth Sciences, St. Petersburg State University, 199034
St. Petersburg, Russia
VNIIOkeangeologia, 190121, St. Petersburg, Russia
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A standardized database compiled to a common format is presented for indicators of sea level during the last interglacial from the southern African coast (Angola, Namibia and South Africa). These enable further analysis of the nature of the sea-level highstand and its regional variability.
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When modelling land uplift processes, there is a need for historical data in which dating, elevation and consequently spatial data are connected to the shore level at that time. In addition, human settlements were located above the seawater level in Fennoscandia. This information can be used to validate and update the post-glacial land uplift model. In this paper, a collection of data consisting of geological and archaeological data sets is presented.
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Short summary
A database of a modern metastable cold-water mineral (ikaite) and its replacement mineral (glendonite) spanning 540 million years has been created to understand their distribution in space and time. A significant body of evidence suggests that glendonite occurrences are restricted mainly to cold-water settings; however they do not occur during every glaciation or cooling event reported from the Phanerozoic. This compilation improves our understanding of climatic conditions of the past.
A database of a modern metastable cold-water mineral (ikaite) and its replacement mineral...
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