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Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus oxygen isotope measurements on Neogloboquadrina pachyderma from Integrated Ocean Drilling Program (IODP) Site U1306 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926659

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Abstract:
The data comprise meters composite depth (mcd) versus oxygen isotope measurements on Neogloboquadrina pachyderma from Integrated Ocean Drilling Program (IODP) Site U130 using a Fisons Optima mass spectrometer at Rutgers University (see Channell et al., 2014). Planktic oxygen isotope (δ18O) and relative paleointensity (RPI) data are used in tandem to generate an age model for the last 1 Myr from Integrated Ocean Drilling Program (IODP) Site U1306 drilled on the crest of the Eirik Drift (SW Greenland) in 2272 m water depth. For the 1-1.5 Ma interval, the age model is based on RPI alone due to insufficient foraminifera for isotope analyses. Utilizing RPI and δ18O in tandem allows recognition of low-δ18O "events" prior to glacial Terminations I, III, IV, V, VII, VIII, IX and X, that are independently supported by radiocarbon dates through the last deglaciation, and are attributed to local or regional surface-water effects. At Site U1306, Quaternary sedimentation rates (mean ~15 cm/kyr) are elevated during peak glacials and glacial onsets, and are reduced during interglacials, in contrast to the pattern at Site U1305 in 3460 m water depth at the distal toe of the drift, 191 km SW of Site U1306. The contrasting sedimentation-rate pattern appears to hold for the entire ~1.5 Myr record. The slackening and/or shoaling (due to lowered salinity) of the Deep Western Boundary Current (DWBC) during glacial intervals coincided with greater sediment supply to Site U1306 whereas the deepening, and possibly increased vigor, of the DWBC during interglacial intervals boosted sediment supply to Site U1305.
Keyword(s):
Deep Western Boundary Current; Eirik Drift; North Atlantic; Oxygen isotopes; Quaternary; relative paleointensity
Related to:
Channell, James E T (2020): Age model of IODP Site 303-U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.919739
Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2014): Age through tandem correlation of Quaternary relative paleointensity (RPI) and oxygen isotope data at IODP Site U1306 (Eirik Drift, SW Greenland). Quaternary Science Reviews, 88, 135-146, https://doi.org/10.1016/j.quascirev.2014.01.022
Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus a relative paleointensity (RPI) proxy (NRM/ARM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926662
Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus component declination, inclination and maximum angular deviation (MAD) values for natural remanent magnetization (NRM) from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926656
Channell, James E T; Wright, James D; Mazaud, Alain; Stoner, Joseph S (2021): Meters composite depth (mcd) versus volume susceptibility and anhysteretic susceptibility from Integrated Ocean Drilling Program (IODP) Site U1306. PANGAEA, https://doi.org/10.1594/PANGAEA.926657
Coverage:
Latitude: 58.208000 * Longitude: -45.630000
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 156.20 m
Event(s):
303-U1306 * Latitude: 58.208000 * Longitude: -45.630000 * Elevation: -2272.0 m * Location: Northwest Atlantic * Campaign: Exp303 (North Atlantic Climate 1) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmChannell, James E TGeocode – mcd
2Neogloboquadrina pachyderma, δ18ON. pachyderma δ18O‰ PDBChannell, James E TMass spectrometer Fisons Optima
Size:
2710 data points

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