Dickens, Gerald Roy; Backman, Jan (2013): (Table S11) Recalibrated depth and ages for previously published stable isotope data from DSDP Hole 86-577 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809200, In supplement to: Dickens, GR; Backman, J (2013): Core alignment and composite depth scale for the lower Paleogene through uppermost Cretaceous interval at Deep Sea Drilling Project Site 577. Newsletters on Stratigraphy, 46(1), 47-68, https://doi.org/10.1127/0078-0421/2013/0027
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Cramer, Benjamin S; Wright, James D; Kent, Dennis V; Aubry, Marie-Pierre (2003): Orbital climate forcing of d13C excursions in the late Paleocene-early Eocene (chrons C24n–C25n). Paleoceanography, 18(4), 1097, https://doi.org/10.1029/2003PA000909
Westerhold, Thomas; Röhl, Ursula; Laskar, Jacques (2012): Time scale controversy: Accurate orbital calibration of early Paleogene. Geochemistry, Geophysics, Geosystems, 13, Q06015, https://doi.org/10.1029/2012GC004096
Westerhold, Thomas; Röhl, Ursula; Raffi, Isabella; Fornaciari, Eliana; Monechi, Simonetta; Reale, Viviana; Bowles, Julie; Evans, Helen F (2008): Astronomical calibration of the Paleocene time. Palaeogeography, Palaeoclimatology, Palaeoecology, 257(4), 377-403, https://doi.org/10.1016/j.palaeo.2007.09.016
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 32.441800 * Longitude: 157.723300
Date/Time Start: 1982-05-23T00:00:00 * Date/Time End: 1982-05-23T00:00:00
Minimum DEPTH, sediment/rock: 74.57 m * Maximum DEPTH, sediment/rock: 87.98 m
Event(s):
86-577 * Latitude: 32.441800 * Longitude: 157.723300 * Date/Time: 1982-05-23T00:00:00 * Elevation: -2675.0 m * Penetration: 118.8 m * Recovery: 111.1 m * Location: North Pacific Ocean * Campaign: Leg86 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 118.8 m cored; 0 m drilled; 93.5 % recovery
Comment:
Placement of previously published bulk and benthic foraminifera stable carbon isotope data for Upper Cretaceous and Lower Paleogene sediment at DSDP Site 577 according to composite depth scale and an updated time scale (Westerhold et al., 2008, 2012). Isotope data were reported by Cramer et al. (2003), dataset doi:10.1594/PANGAEA.741861. DEPTH, sediment is the depth [mbsf] reported by Cramer et al. (2003). Note that depths for CC samples are not consistent with core logs.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Dickens, Gerald Roy | DSDP/ODP/IODP sample designation | we have relabled core catcher (CC) samples as an additional section for purposes of math; given in brackets | |
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Depth, top/min | Depth top | m | Dickens, Gerald Roy | core top [mbsf], reported according to drillers table (Shipboard Scientific Party, 1985) and with positions of CC intervals from core logs | |
4 | Void correction | Void corr | m | Dickens, Gerald Roy | ||
5 | Depth, sediment revised | Depth revised | m | Dickens, Gerald Roy | corrected [mbsf], assuming average interval distance and the above | |
6 | Offset | Offset | m | Dickens, Gerald Roy | offset of cores from Table 2 | |
7 | Depth, composite | Depth comp | mcd | Dickens, Gerald Roy | adjusted, the depth of the sample in floating depth space [mcd] relative to m below seafloor | |
8 | δ13C, carbonate | δ13C carb | ‰ PDB | Cramer, Benjamin S | ||
9 | δ18O, carbonate | δ18O carb | ‰ PDB | Cramer, Benjamin S | ||
10 | Age, relative | Age rel | ka | Cramer, Benjamin S | reported age relative to start of PETM reported by Cramer et al. (2003) | |
11 | Age model | Age model | ka | Dickens, Gerald Roy | estimated age on Option 1 time by Westerhold et al. (2008) as determined by linear sedimentaton between six polarity chron reversals and data on a mcd depth scale | |
12 | Age, relative | Age rel | ka | Dickens, Gerald Roy | estimated age relative to start of PETM using information in this paper | |
13 | Comment | Comment | Dickens, Gerald Roy | Blue horizons are approximate positions of polarity chron reversals; green horizons are positions of known hyperthermal events. Note that ages given for hyperthermals differ from those estimated, which may reflect inaccurate ages for the hyperthermals or differential sedimentation between chosen polarity chrons. |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
6140 data points
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