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Gorbarenko, Sergey A; Tsoy, Ira B; Astakhov, Anatolii S; Artemova, Antonina V; Gvozdeva, I G; Annin, V K; Rasskazov, S V (2007): Ages of sediments from Core MG34-89211, northern shelf of the Sea of Okhotsk [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.745157, Supplement to: Gorbarenko, Sergey A; Tsoy, Ira B; Astakhov, Anatolii S; Artemova, Antonina V; Gvozdeva, I G; Annin, V K (2007): Paleoenvironmental changes in the northern shelf of the Sea of Okhotsk during the Holocene. Stratigraphy and Geological Correlation, 15(6), 656-671, https://doi.org/10.1134/S0869593807060044

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Published: 2007 (exact date unknown)DOI registered: 2010-10-11

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Abstract:
The combined micropaleontological (spores and pollen, diatoms, benthic foraminifers), lithologic, and isotopic-geochemical analysis of sediments from the northern shelf of the Sea of Okhotsk recovered by hydrostatic corer from the depth of 140 mbsl elucidated environmental changes in this part of the basin and adjacent land areas during the last 12.7 thousands cal. years. Geochronological scale of the core is established using the acceleration mass-spectrometry method for radiocarbon dating of benthic Foraminifera tests. The first insignificant warming in the northern part of the sea after glaciation occurred in the mid-Boreal time (9.6 ka ago) but not at the onset of the Holocene. The strongest warming in the region took place in the mid-Atlantic epoch to reach climatic optimum in the second half of the Subboreal (6 to 2.5 ka ago). A cooling in the northern shelf and adjacent land areas is established at the beginning of the Subatlantic (2.5 ka). A comparison of results obtained for Core 89211 with dated hydrological and climatic changes in central and southern parts of the Sea of Okhotsk (Gorbarenko et al., 2003, 2004) is used for a high-resolution analysis of climatic fluctuations in the study region and other areas of the basin during deglaciation and the Holocene.
Project(s):
Coverage:
Latitude: 58.583333 * Longitude: 145.470000
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 1.94 m
Event(s):
MG34-89211 * Latitude: 58.583333 * Longitude: 145.470000 * Elevation: -140.0 m * Location: Sea of Okhotsk * Campaign: MG34 * Basis: Morskoy Geophysik * Method/Device: Box corer (BC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Sample, optional label/labor noLab noRasskazov, S V
Sample typeSamp typeRasskazov, S V
Age, datedAge datedkaRasskazov, S V
Age, dated, standard deviationAge dated std dev±Rasskazov, S VCalculated
Age, datedAge datedkaRasskazov, S VAge, 14C milieu/reservoir correctedcorrected for reservoir age of surface waters in the Sea of Okhotsk (900 years)
Calendar ageCal ageka BPRasskazov, S VAge, 14C milieu/reservoir correctedcalibrated after Bard (1998; doi:10.1016/S0016-7037(98)00130-6)
Analytical methodAnalyt methodRasskazov, S V
Size:
63 data points

Data

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Depth sed [m]

Lab no

Samp type

Age dated [ka]

Age dated std dev [±]
(Calculated)

Age dated [ka]
(corrected for reservoir age o...)

Cal age [ka BP]
(calibrated after Bard (1998; ...)

Analyt method
0.05CAMS-66138N. pachydermas (Ehrenberg)0.870.050.000.158accelerator mass spectrometry
0.70OS-11668Benthic foraminifers6.600.055.706.491accelerator mass spectrometry
0.80CAMS-71877Islandiella japonica7.300.056.407.250accelerator mass spectrometry
1.10OS-11667Benthic foraminifers8.030.067.138.010accelerator mass spectrometry
1.30CAMS-71878Islandiella japonica8.200.057.308.188accelerator mass spectrometry
1.40OS-16710Cassidulina subacuta8.660.067.768.666accelerator mass spectrometry
1.94CAMS-66139Benthic foraminifers11.870.0610.9712.780accelerator mass spectrometry
1.58KI-3753Molluscan shells8.900.078.008.900radiocarbon dating
1.93KI-3754Molluscan shells14.200.0913.3015.650radiocarbon dating