Cretaceous to Recent Uplift Measurements from Marine Fossil Assemblages

Cretaceous to Recent marine assemblages (total of 24,372) used to measure uplift, interpreted paleo-water depths and measured uplift. This inventory contains information about age, location, stratigraphic origin (i.e., formation, unit, member), lithology, paleoenvironment, and tectonic setting at the time of deposition and references to original source material. An extended methodology is presented in, Victoria M. Fernandes, Gareth G. Roberts; Cretaceous to Recent net continental uplift from paleobiological data: Insights into sub-plate support. GSA Bulletin 2020;; 133 (5-6): 1217–1236. doi: https://doi.org/10.1130/B35739.1 Examples of this information being used to test mantle convection simulations is presented in, Victoria, M. Fernandes, Gareth G. Roberts, Fred Richards; Testing Mantle Convection Simulations With Paleobiology and Other Stratigraphic Observations: Examples From Western North America. G-Cubed 2024; 25(e2023GC011381). doi: https://doi.org/10.1029/2023GC011381

Date (Creation): 2024-08-13

Identifier: http://data.bgs.ac.uk/id/dataHolding/13608265

Originator

Imperial College London - Gareth Roberts

Department of Earth Science and Engineering, Imperial College London, South Kensington Campus , London , SW7 2AZ ,

Originator

Imperial College London - Victoria Fernandes

Distributor

British Geological Survey - Enquiries

Point of contact

British Geological Survey - Enquiries

Maintenance and update frequency: notApplicable notApplicable

GEMET - INSPIRE themes, version 1.0

Geology

BGS Thesaurus of Geosciences

Cenozoic
Uplift
NGDC Deposited Data
Cretaceous

dataCentre

NGDC Deposited Data

Keywords

NERC_DDC

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Other constraints: licenceOGL

Other constraints: Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]"

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Other constraints: The copyright of materials derived from the British Geological Survey's work is vested in the Natural Environment Research Council [NERC]. No part of this work may be reproduced or transmitted in any form or by any means, or stored in a retrieval system of any nature, without the prior permission of the copyright holder, via the BGS Intellectual Property Rights Manager. Use by customers of information provided by the BGS, is at the customer's own risk. In view of the disparate sources of information at BGS's disposal, including such material donated to BGS, that BGS accepts in good faith as being accurate, the Natural Environment Research Council (NERC) gives no warranty, expressed or implied, as to the quality or accuracy of the information supplied, or to the information's suitability for any use. NERC/BGS accepts no liability whatever in respect of loss, damage, injury or other occurence however caused.

Other constraints: Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]"

Spatial representation type: vector Vector

Metadata language: EnglishEnglish

Topic category

Geoscientific information

Begin date: 2019-07-08

End date: 2020-08-08

Unique resource identifier: WGS 84 (EPSG::4326)

Distribution format

txt ()

Distributor

British Geological Survey - Enquiries

OnLine resource: Digital Object Identifier (DOI)

OnLine resource: Data

Hierarchy level: dataset Dataset

Other: dataset

Conformance result

Date (Publication): 2011

Explanation: See the referenced specification

Pass: No

Conformance result

Date (Publication): 2010-12-08

Explanation: See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF

Pass: No

Statement: Fossil occurrences were retrieved from the Paleobiology Database (PBDB) on 8 July 2019 using the following filters: Maximum Age = 100.5 Ma, Minimum Age = 0 Ma (Cenomanian to Recent). This inventory contains information about age, location, stratigraphic origin (i.e., formation, unit, member), lithology, paleoenvironment, and tectonic setting at the time of deposition and references to original source material. Non-marine fossils were removed, fossil locations were corrected where necessary, and qualitative paleoenvironmental information was converted into quantitative estimates of paleobathymetry. An extended methodology is presented in Fernandes & Roberts (2020).