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Bartoli, Gretta; Hönisch, Bärbel; Zeebe, Richard E (2011): (Table S1) Globigerinoides sacculifer Boron isotope ratios of ODP Hole 165-999A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.829486, Supplement to: Bartoli, G et al. (2011): Atmospheric CO2 decline during the Pliocene intensification of Northern Hemisphere glaciations. Paleoceanography, 26(4), PA4213, https://doi.org/10.1029/2010PA002055

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Abstract:
everal hypotheses have been put forward to explain the onset of intensive glaciations on Greenland, Scandinavia, and North America during the Pliocene epoch between 3.6 and 2.7 million years ago (Ma). A decrease in atmospheric CO2 may have played a role during the onset of glaciations, but other tectonic and oceanic events occurring at the same time may have played a part as well. Here we present detailed atmospheric CO2 estimates from boron isotopes in planktic foraminifer shells spanning 4.6-2.0 Ma. Maximal Pliocene atmospheric CO2 estimates gradually declined from values around 410 µatm to early Pleistocene values of 300 matm at 2.0 Ma. After the onset of large-scale ice sheets in the Northern Hemisphere, maximal pCO2 estimates were still at 2.5 Ma +90 µatm higher than values characteristic of the early Pleistocene interglacials. By contrast, Pliocene minimal atmospheric CO2 gradually decreased from 310 to 245 µatm at 3.2 Ma, coinciding with the start of transient glaciations on Greenland. Values characteristic of early Pleistocene glacial atmospheric CO2 of 200 matm were abruptly reached after 2.7 Ma during the late Pliocene transition. This trend is consistent with the suggestion that ocean stratification and iron fertilization increased after 2.7 Ma in the North Pacific and Southern Ocean and may have led to increased glacial CO2 storage in the oceanic abyss after 2.7 Ma onward.
Project(s):
Coverage:
Latitude: 12.744000 * Longitude: -78.739300
Date/Time Start: 1996-01-10T19:30:00 * Date/Time End: 1996-01-14T23:15:00
Minimum DEPTH, sediment/rock: 64.74 m * Maximum DEPTH, sediment/rock: 140.78 m
Event(s):
165-999A * Latitude: 12.744000 * Longitude: -78.739300 * Date/Time Start: 1996-01-10T19:30:00 * Date/Time End: 1996-01-14T23:15:00 * Elevation: -2828.0 m * Penetration: 566.1 m * Recovery: 534.83 m * Location: Caribbean Sea * Campaign: Leg165 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 61 core; 566.1 m cored; 0 m drilled; 94.5 % recovery
Comment:
DEPTH, sediment/rock is given in mbsf.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelBartoli, GrettaDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode
3AGEAgeka BPGeocode
4Size fractionSize fractionBartoli, Grettain µm
5Isotopic eventIsotopic eventBartoli, Gretta
6Method commentMethod commBartoli, Gretta
7Globigerinoides sacculifer, weightG. sacculifer WµgBartoli, Gretta
8Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 1
9Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 2
10Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 3
11Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 4
12Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 5
13Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettarun 6
14Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettaoutliers
15Globigerinoides sacculifer, δ11BG. sacculifer δ11B‰ SRMBartoli, Grettaaveraged d11B w/out outliers
16Globigerinoides sacculifer, δ11B, standard errorG. sacculifer δ11B std e±Bartoli, Grettainternal uncertainty (2se)
17Globigerinoides sacculifer, δ11B, standard errorG. sacculifer δ11B std e±Bartoli, Grettaexternal reproducibility (2se) of vaterite for same number of runs
18Globigerinoides sacculifer, δ11B, standard errorG. sacculifer δ11B std e±Bartoli, Grettaplotted error-bars
Size:
659 data points

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