(Table 1) Age determination on monospecies planktonic foraminifera of sediment core AN25-934, supplement to: Gorbarenko, Sergey A; Artemova, Antonina V; Goldberg, Evgeniy L; Vasilenko, Yuriy P (2014): The response of the Okhotsk Sea environment to the orbital-millennium global climate changes during the Last Glacial Maximum, deglaciation and Holocene. Global and Planetary Change, 116, 76-90

• Main Authors: Gorbarenko, Sergey A, Artemova, Antonina V, Goldberg, Evgeniy L, Vasilenko, Yuriy P
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2014
• Subjects: Sample, optional label/labor no; DEPTH, sediment/rock; Age, dated material; Age, dated; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; Gravity corer; Age, 14C AMS; Age, 14C calibrated, CALIB 6.0 and Marine09 Reimer et al., 2009; Okhotsk; Greenland; Pacific; Reimer; Greenland ice core; Greenland ice cores; ice core; North Atlantic; okhotsk sea; Planktonic foraminifera; Sea ice
• Online Access: https://dx.doi.org/10.1594/pangaea.829761; https://doi.pangaea.de/10.1594/PANGAEA.829761

Reconstruction of regional climate and the Okhotsk Sea (OS) environment for the Last Glacial Maximum (LGM), deglaciation and Holocene were performed on the basis of high-resolution records of ice rafted debris (IRD), CaCO3, opal, total organic carbon (TOC), biogenic Ba (Ba_bio) and redox sensitive element (Mn, Mo) content, and diatom and pollen results of four cores that form a north-southern transect. Age models of the studied cores were earlier established by AMS 14C data, oxygen - isotope chronostratigraphy and tephrochronology. According to received results, since 25 ka the regional climate and OS environmental conditions have changed synchronously with LGM condition, cold Heinrich event 1, Bølling -Allerød (BA) warming, Younger Dryas (YD) cooling and Pre-Boreal (PB) warming recorded in the Greenland ice core, North Atlantic sediment, and China cave stalagmites. Calculation of IRD MAR in sediment of north-south transect cores indicate an increase of sea ice formation several times in the glacial OS as compared to the Late Holocene. Accompanying ice formation, increased brine rejection and the larger potential density of surface water at the north shelf due to a drop of glacial East Asia summer monsoon precipitation and Amur River run off, led to strong enhancement of the role of the OS in glacial North Pacific Intermediate Water (NPIW) formation. The remarkable increase in OS productivity during BA and PB warming was probably related with significant reorganisation of the North Pacific deep water ventilation and nutrient input into the NPIW and OS Intermediate Water (OSIW). Seven Holocene OS millennial cold events based on the elevated values of the detrended IRD stack record over the IRD broad trend in the sediments of the studied cores have occurred synchronously with cold events recorded in the North Atlantic, Greenland ice cores and China cave stalagmites after 9 ka. Diatom production in the OS were mostly controlled by sea ice cover changes and surface water stratification induced by sea-ice melting; therefore significant opal accumulation in sediments of this basin begin from 4-6 ka ago simultaneously with a remarkable decrease of sea ice cover. : Measured 14C age data were corrected by Okhotsk Sea surface water reservoir ages equal to Delta R=550±250 yr. Radiocarbon-calendar age conversion was performed by using the calibration tool Calib Rev 6.0 (Stuiver and Reimer, 1993) with the Marine 09 data sets (Hughen et al., 2004; Reimer et al., 2009).