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Kristjánsdóttir, Greta B; Moros, Matthias; Andrews, John T; Jennings, Anne E (2015): (Appendix I) Stable isotope measurements of benthic and planktonic foraminifera in sediment core MD99-2269 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.847652, In supplement to: Kristjánsdóttir, GB et al. (2016): Holocene Mg/Ca, alkenones, and light stable isotope measurements on the outer North Iceland shelf (MD99-2269): A comparison of proxy data. The Holocene, 27(1), 52-62, https://doi.org/10.1177/0959683616652703

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Related to:
Kristjánsdóttir, Greta B (2005): Holocene climatic and environmental changes on the Iceland shelf: d18O, Mg/Ca, and tephrochronology of core MD99-2269. Ph.D. thesis, University of Colorado at Boulder, 423 pp.
Coverage:
Latitude: 66.641333 * Longitude: -20.863167
Date/Time Start: 1999-08-01T00:00:00 * Date/Time End: 1999-08-01T00:00:00
Minimum DEPTH, sediment/rock: 0.06 m * Maximum DEPTH, sediment/rock: 25.29 m
Event(s):
MD99-2269 (79US/Fr) * Latitude: 66.641333 * Longitude: -20.863167 * Date/Time: 1999-08-01T00:00:00 * Elevation: -365.0 m * Recovery: 25.44 m * Location: N.Iceland shelf, Reykjafjardarall * Campaign: MD114 (IMAGES V) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO)
Comment:
Isotopic analysis was performed at the Leibniz-Laboratory for radiometric dating and stable isotope research at Christian-Albrechts-University Kiel, Germany using a Finnigan MAT 251 mass spectrometer with an on-line coupled Kiel Carbon device. First 13 columns are raw data as reported from the Kiel laboratory, samples with warnings and/or remarks are " shown with full remarks at the end of this Appendix. The ± errors in the data sheets is the internal error. Each sample is measured ten times (in a succession of reference gas, sample gas, reference gas, sample gas etc.). The internal error is the SD of the ten measurements of the sample gas. If the sample size is very" small then the internal error will be increased. The external error (also called the analytical error) measures how accurately carbonate standards can be reproduced (by comparison of the resulting values which base each on ten internal measurements). Different carbonates are used as standards and measured regularly each day in the lab and results checked for performance of the mass spec, but generally not sent to the customers. For a sample > 15 µg the external error is better than 0.04 per mil (13C) and 0.06 per mil (18O). For smaller sizes the error is higher, going up to 0.2 per mil for < 8 µg. However, these small sample sizes are signed with warnings in the data sheets. For the earliest sample batch of Nps two morphotypes were run separately; Nps quadrate form (Npsq) and Nps normal form (Npsn). Sample depth is shown on both original depth scale (cm*) and void corrected depth scale (cm). For depths with multiple measurements an average was used for data analysis, the average is not shown in this Appendix, only the separate original values.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1NumberNoAndrews, John T
2Run Date/TimeRun Date/TimeAndrews, John Tmeasured
3Run Date/TimeRun Date/TimeAndrews, John Tloaded
4PositionPositionAndrews, John T
5CommentCommentAndrews, John Twarning
6--Andrews, John TAI
7MassMassµgAndrews, John TSaSi
8Cibicides lobatulus, δ13CC. lobatulus δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
9Cibicides lobatulus, δ13C standard deviationC. lobatulus δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251
10Cibicides lobatulus, δ18OC. lobatulus δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
11Cibicides lobatulus, δ18O standard deviationC. lobatulus δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251
12Cassidulina neoteretis, δ13CC. neoteretis δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
13Cassidulina neoteretis, δ13C standard deviationC. neoteretis δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251
14Cassidulina neoteretis, δ18OC. neoteretis δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
15Cassidulina neoteretis, δ18O standard deviationC. neoteretis δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251
16Globigerina quinqueloba, δ13CG. quinqueloba δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
17Globigerina quinqueloba, δ13C standard deviationG. quinqueloba δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251
18Globigerina quinqueloba, δ18OG. quinqueloba δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
19Globigerina quinqueloba, δ18O standard deviationG. quinqueloba δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251
20Islandiella norcrossi, δ13CI. norcrossi δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251Islandiella norcrossi/helenae
21Islandiella norcrossi, δ13C standard deviationI. norcrossi δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251Islandiella norcrossi/helenae
22Islandiella norcrossi, δ18OI. norcrossi δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251Islandiella norcrossi/helenae
23Islandiella norcrossi, δ18O standard deviationI. norcrossi δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251Islandiella norcrossi/helenae
24Melonis barleeanus, δ13CM. barleeanus δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
25Melonis barleeanus, δ13C standard deviationM. barleeanus δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251
26Melonis barleeanus, δ18OM. barleeanus δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251
27Melonis barleeanus, δ18O standard deviationM. barleeanus δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251
28Neogloboquadrina pachyderma sinistral, δ13CN. pachyderma s δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251total
29Neogloboquadrina pachyderma sinistral, δ13C standard deviationN. pachyderma s δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251total
30Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251total
31Neogloboquadrina pachyderma sinistral, δ18O standard deviationN. pachyderma s δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251total
32Neogloboquadrina pachyderma sinistral, δ13CN. pachyderma s δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251normal form
33Neogloboquadrina pachyderma sinistral, δ13C standard deviationN. pachyderma s δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251normal form
34Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251normal form
35Neogloboquadrina pachyderma sinistral, δ18O standard deviationN. pachyderma s δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251normal form
36Neogloboquadrina pachyderma sinistral, δ13CN. pachyderma s δ13C‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251quadrate form
37Neogloboquadrina pachyderma sinistral, δ13C standard deviationN. pachyderma s δ13C std dev±Andrews, John TMass spectrometer Finnigan MAT 251quadrate form
38Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBAndrews, John TMass spectrometer Finnigan MAT 251quadrate form
39Neogloboquadrina pachyderma sinistral, δ18O standard deviationN. pachyderma s δ18O std dev±Andrews, John TMass spectrometer Finnigan MAT 251quadrate form
40Laboratory code/labelLab labelAndrews, John T
41Comment 2 (continued)Comm 2Andrews, John T# caution; sample very small; yet managed by the machine; see #1 if a small sample is processed, pressure adjustment may become established in the early phase of a reference gas cycle (which is consumed during machine operation and is renewed every 8 to 10 samples), but could be reached in the later phase. A bad pressure adjustment may produce an isotope offset which however is not reproducible with sufficient precision. may suffer a bit (0.2...0.4 per mil in d18O) from too low a sample size or from machine problems
42Depth, top/minDepth topmAndrews, John Toriginal depth scale
43Depth, top/minDepth topmAndrews, John Tvoid corrected depth scale
44ShellShell#Andrews, John Trefers to the number of tests run
45PyritePyAndrews, John TPresence (x) or absence () in the sampels. For a few samples the number of tests with pyrite in them is shown. Pyrite was not checked in the earliest sample batch (Na).
46DEPTH, sediment/rockDepth sedmAndrews, John TGeocode – Mid depth, original depth scale
47Depth, sediment revisedDepth revisedmAndrews, John TMid depth, void corrected depth scale
Size:
10531 data points

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