Sabino, Mathia; Dela Pierre, Francesco; Natalicchio, Marcello; Birgel, Daniel; Gier, Susanne; Peckmann, Jörn (2021): Carbon and oxygen stable isotopes of the Govone section [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.927058, In: Sabino, M et al. (2021): Changes in water column and sedimentary environments at the onset of the Messinian salinity crisis: Insights from an onshore deep-water section (Govone, NW Italy) [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.927059
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2021-01-27 • DOI registered: 2021-02-27
Keyword(s):
Related to:
Sabino, Mathia; Dela Pierre, Francesco; Natalicchio, Marcello; Birgel, Daniel; Gier, Susanne; Peckmann, Jörn (2020): The response of water column and sedimentary environments to the advent of the Messinian salinity crisis: insights from an onshore deep-water section (Govone, NW Italy). Geological Magazine, 1-17, https://doi.org/10.1017/S0016756820000874
Further details:
Bernardi, E (2013): Integrated stratigraphy of the northernmost record of the Messinian salinity crisis: new insights from the Tertiary Piedmont Basin [dissertation]. University of Torino, Torino, Italy. Published thesis
Kim, Sang-Tae; Mucci, Alfonso; Taylor, Bruce (2007): Phosphoric acid fractionation factors for calcite and aragonite between 25 and 75 °C: Revisited. Chemical Geology, 246(3-4), 135-146, https://doi.org/10.1016/j.chemgeo.2007.08.005
Rosenbaum, J; Sheppard, S M F (1986): An isotopic study of siderites, dolomites and ankerites at high temperatures. Geochimica et Cosmochimica Acta, 50(6), 1147-1150, https://doi.org/10.1016/0016-7037(86)90396-0
Sharma, Taleshwar; Clayton, Robert N (1965): Measurement of ratios of total oxygen of carbonates. Geochimica et Cosmochimica Acta, 29(12), 1347-1353, https://doi.org/10.1016/0016-7037(65)90011-6
Coverage:
Latitude: 44.802222 * Longitude: 8.126111
Minimum SECTION, height: 37.11 m * Maximum SECTION, height: 42.31 m
Comment:
* samples from Bernardi, 2013
Correction factors for δ18O values:
Samples from Bernardi (2013) were corrected by −0.8‰ according to Sharma & Clayton (1965) for analyses performed at T= 323.15 °K. The new samples were corrected for −1.2‰. This values was obtained as the difference between the fractionation among CO2 and solid dolomite according to Rosenbaum & Sheppard, (1986) (10^3lnα = 6.65 x 10^5 x (1/T^2) + 4.23) and CO2 and solid calcite according to Kim et al (2007) (10^3lnα = 3.59 x (10^3/T) - 1.79) for a reaction temperature of T= 348.15 °K.
Errors related to analyses performed by Bernardi et al. (2013): δ13C = ±0.5‰ ; δ18O = ±0.1‰
Errors related to analyses presented in this study: δ13C = ±0.04‰ ; δ18O = ±0.06‰
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Sabino, Mathia | |||
| 2 | Sample comment | Sample comment | Sabino, Mathia | |||
| 3 | SECTION, height | Section | m | Sabino, Mathia | Geocode | |
| 4 | Cycle | Cy | Sabino, Mathia | |||
| 5 | δ13C, carbonate | δ13C carb | ‰ PDB | Sabino, Mathia | Finnigan MAT 252 gas isotope ratio mass spectrometer with Kiel III automated carbonate preparation device | |
| 6 | δ18O, carbonate | δ18O carb | ‰ PDB | Sabino, Mathia | Finnigan MAT 252 gas isotope ratio mass spectrometer with Kiel III automated carbonate preparation device |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
145 data points
Data
| 1 Sample label | 2 Sample comment | 3 Section [m] | 4 Cy | 5 δ13C carb [‰ PDB] | 6 δ18O carb [‰ PDB] |
|---|---|---|---|---|---|
| Gm33.2 | Shale | 42.31 | Gm 33 | -4.3 | 3.4 |
| Gm32.6 | Marl | 42.07 | Gm 32 | -4.2 | 3.5 |
| Gm32.5 | Marl | 41.80 | Gm 32 | -2.6 | 4.7 |
| GM 32.2* | Marl | 41.78 | Gm 32 | -5.2 | 2.9 |
| Gm32.4 | Marl | 41.56 | Gm 32 | -4.2 | 5.5 |
| Gm32.3 | Shale | 41.47 | Gm 32 | -2.8 | 5.4 |
| GM 32.1* | Shale | 41.27 | Gm 32 | -1.4 | 2.9 |
| Gm31.5 | Marl | 41.06 | Gm 31 | -0.4 | 3.6 |
| GM 31.1* | Marl | 41.00 | Gm 31 | -0.4 | 3.7 |
| GOV B 12.1* | Marl | 40.77 | Gm 31 | -4.4 | 5.1 |
| Gm31.3 | Marl | 40.75 | Gm 31 | -1.5 | 4.9 |
| Gm31.2 | Shale | 40.63 | Gm 31 | -0.8 | 3.2 |
| GOV B 11.4* | Shale | 40.46 | Gm 31 | -0.9 | -3.1 |
| GOV B 11.2* | Marl | 40.16 | Gm 30 | -0.4 | 3.8 |
| GOV B 10.5* | Shale | 39.91 | Gm 30 | -1.4 | 4.9 |
| GOV B 10.4* | Shale | 39.87 | Gm 30 | -0.4 | 2.6 |
| GOV B 10.3* | Marl | 39.75 | Gm 29 | -0.4 | 3.8 |
| Gm29.3 | Marl | 39.59 | Gm 29 | -2.7 | 4.9 |
| GM 29* | Marl | 39.48 | Gm 29 | -2.3 | 5.1 |
| GOV B 9.4* | Shale | 39.41 | Gm 29 | -0.9 | 5.0 |
| GOV B 9.3* | Marl | 39.21 | Gm 28 | -1.3 | 4.9 |
| GOV B 9.2* | Marl | 39.00 | Gm 28 | 0.3 | 0.0 |
| GOV B 9.1* | Marl | 38.86 | Gm 28 | -2.2 | 4.9 |
| GOV B 8.2* | Marl | 38.24 | Gm 27 | 0.3 | -4.3 |
| GOV B 8.1* | Marl | 38.03 | Gm 27 | -0.4 | -0.3 |
| GOV B 7.4* | Shale | 37.86 | Gm 27 | -1.7 | 2.5 |
| GOV B 7.3* | Marl | 37.54 | Gm 26 | 0.3 | -4.5 |
| GOV B 7.2* | Marl | 37.31 | Gm 26 | -2.1 | 5.4 |
| GOV B 7.1* | Shale | 37.11 | Gm 26 | -0.2 | -3.9 |