cff3e1df-e00f-65a3-e054-002128a47908 English nonGeographicDataset non geographic dataset British Geological Survey +44 115 936 3100 Environmental Science Centre,Keyworth NOTTINGHAM NOTTINGHAMSHIRE NG12 5GG United Kingdom enquiries@bgs.ac.uk pointOfContact 2026-04-15 UK GEMINI 2.3 http://data.bgs.ac.uk/id/dataHolding/13607834 Terrestrial palaeo-environmental proxy data of the Upper Pliensbachian, Mochras Borehole sediments, deposited in the Cardigan Bay Basin, Wales (NERC Grant NE/N018508/1) 2021-10-12 creation http://data.bgs.ac.uk/id/dataHolding/13607834 Terrestrial palaeo-environmental proxy data has been collected to examine orbital changes in wildfire activity in the Early Jurassic of the Mochras Borehole, Cardigan Bay Basin, Wales. To do this a high resolution charcoal abundance dataset was created and quantified in two size fractions, microscopic charcoal (10-125 µ) and macroscopic charcoal (>125 µ). To take potential changes in riverine influx and/or organic preservation in account on the charcoal abundance, palynofacies were analysed to document all terrestrial and marine organic particles present in the samples, and next to this, X-ray fluorescence data was gathered to assess detrital output. Mass spectrometry provided information on the carbonate and Total Organic Carbon content and bulk organic carbon isotopes. This information was used to look at changes in the lithology and the carbon cycle. Finally, clay mineralogical data was obtained to look at changes in the hydrological cycle in relation to wildfire activity. This dataset spans 951-934 mbs from the Mochras borehole, which is the time equivalent of ~350 kyr, in the Margaritatus Zone of the Upper Pliensbachian. The Mochras sediments have been deposited in the Cardigan Bay Basin, Wales. At the time of deposition, this location was positioned in the Laurasian Seaway at a paleolatitude of ~35°N. These datasets were obtained at a high resolution (10 cm) using X-ray diffraction, X-ray fluorescence, mass spectrometry and palynological preparations. This high resolution was acquired to analyse the presence of precessional orbital forcing on wildfire and the other proxy datasets. This data was collected, interpreted and analysed by Teuntje Hollaar, Claire Belcher, Stephen Hesselbo, Micha Ruhl, Jean-Franҫois Deconinck, Sarah Jane Baker and Luke Mander. The complete dataset presented in the published article file ‘Wildfire activity enhanced during phases of maximum orbital eccentricity and precessional forcing in the Early Jurassic’ has been included in this data file. Stephen Hesselbo University of Exeter Camborne School of Mines Penryn Campus Penryn Cornwall TR10 9FE not available principalInvestigator Teuntje Hollaar University of Exeter PhD student Laver Building, North Park Road Exeter EX4 4QE not available originator Enquiries British Geological Survey United Kingdom not available distributor Enquiries British Geological Survey United Kingdom not available pointOfContact notApplicable https://resources.bgs.ac.uk/images/geonetworkThumbs/cff3e1df-e00f-65a3-e054-002128a47908.png Geology GEMET - INSPIRE themes, version 1.0 2008-06-01 publication Charcoal X ray diffraction Clay mineralogy TOC Mass spectroscopy X ray fluorescence spectroscopy Carbonates Jurassic BGS Thesaurus of Geosciences 2022 revision NGDC Deposited Data Citable Data dataCentre NERC_DDC otherRestrictions licenceOGL Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]" otherRestrictions 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. Available under the Open Government Licence subject to the following acknowledgement accompanying the reproduced NERC materials "Contains NERC materials ©NERC [year]" English geoscientificInformation 2017-12-01 2020-02-01 Microsoft Excel witheld Enquiries British Geological Survey United Kingdom not available distributor https://doi.org/10.5285/d6b7c567-49f0-44c7-a94c-e82fa17ff98e WWW:LINK-1.0-http--related Citation Information - Digital Object Identifier (DOI) information https://webapps.bgs.ac.uk/services/ngdc/accessions/index.html#item169090 WWW:DOWNLOAD-1.0-http--download Data download nonGeographicDataset non geographic dataset INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology 2011 publication See the referenced specification false Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services 2010-12-08 publication See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF false XRD Powdered bulk rock samples were decarbonated with a 0.2 M HCl solution. The clay size fraction was extractedand analysed by X-ray diffraction. The clay phases were discriminated in three runs per sample: 1) air-drying at room temperature; 2) ethylene-glycol solvation during 24 hours; 3) heating at 490°C during 2 hours. XRF Elemental concentrations were obtained by automated X-ray XRF analyses were conducted with the ITRAX MC, with a 30-sec measurement window. Long-term drift in the measurement values was counteracted by regular internal calibration with a glass reference. Additionally, every 5 metre, a 30 cm interval was duplicated. Mass spectrometry Powdered bulk rock samples were decarbonized using 3.3% HCl and given a hot bath of 79°C for 1 h to remove siderite and dolomite. The neutralized samples were weighted in tin capsules for mass spectrometry.