Stable Isotope and geochemical Data from Spain and France (NERC grant NE/J020842/1)
Stable Isotope and trace element analyses (Ca, Sr, Mg, Fe and Mn concentrations) derived from Cretaceous Belemnites including Duvalia tornajoensis, D. cf. lata constricta, D. binervia, D. cf. emericii, Hibolithes, H. cf. jaculoides, Berriasibelus, Castellanibelus and Pseudobelus.
dataset
http://www.bgs.ac.uk/services/ngdc/accessions/index.html#item110891
function: download
http://data.bgs.ac.uk/id/dataHolding/13607343
eng
The belemnites are dervied from sections in Spain, located near Caravaca and Cehegín: Prado Borda Section, 2.1 km SSE of Caravaca (38°0513°N 1°5114°W); Sections on the north-eastern slope of Mai Valera Mountain, 2 km W of Cehegín (38°0539°N 1°4909°W), Sections along the Cañada Luenga ravine, 3.1 km SSW of Cehegín (38°0402°N 1°4849°W), and the Barranco del Garranchal Section, 5.5 km SSW of Cehegín (38°0242°N 1°4920°W). The belemnites from France are from the La Charce section (44°2809°N 5°2637°W), the Vergol/Morénas section(44°1212°N 5°2509°W), and the Angles Section (43°5628°N 6°3232°W).
geoscientificInformation
publication
2008-06-01
Carbon isotopes
Oxygen isotopes
Cretaceous
Trace analysis
Stable isotopes
Fossils
revision
2011
NERC_DDC
5.4100
6.5500
44.4700
43.9400
revision
2009
ES
revision
2009
ESP
revision
2009
FR
revision
2009
FRA
creation
1979
FRANCE [id=210000]
creation
1979
SPAIN [id=248000]
2016-12-01
2017-12-28
creation
2018-06-19
notApplicable
The belemnites were prepared for stable isotope & trace element analysis by first removing the areas of the rostrum typically most prone to diagenesis. The remaining calcite was then fragmented, washed in ultrapure (Type 1) water and dried in a clean environment. Using 300 to 400 micrograms of carbonate, stable isotope data were generated on a VG Optima mass spectrometer with a Gilson autosampler at the University of Plymouth. Isotope ratios were calibrated using NBS standards and are given in δ notation relative to the Vienna Pee Dee Belemnite (V-PDB). Reproducibility was generally better than 0.1‰ for samples and standard materials. The sub-samples taken for trace element analysis were digested in HNO3 and analysed by Inductively Coupled Plasma-Atomic Emission Spectrometer (ICP-AES) using a PerkinElmer 3100 at the University of Plymouth.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
MS Excel
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School of Geography, Earth and Environmental Sciences
University of Plymouth
Fitzroy, Drake Circus
Plymouth
PL4 8AA
pointOfContact
School of Geography, Earth and Environmental Sciences
University of Plymouth
Fitzroy, Drake Circus
Plymouth
PL4 8AA
principalInvestigator
British Geological Survey
Environmental Science Centre,Keyworth
NOTTINGHAM
NG12 5GG
United Kingdom
+44 115 936 3100
pointOfContact
2023-05-24