Barium Increasing prior to Opal during the Last Termination of Glacial Ages in the Okhotsk Sea Sediments

• Main Authors: Masayasu M. Sato, Hisashi Narita, Shizuo Tsunogai
• Other Authors: The Pennsylvania State University CiteSeerX Archives
• Format: Text
• Language: English
• Published: 2001
• Subjects: Okhotsk; okhotsk sea
• Online Access: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.424.6756; http://www.terrapub.co.jp/journals/JO/pdf/5803/58030461.pdf

Ba and Ti in a sediment core (10 m long) from the Okhotsk Sea, covering the last 120 kyrs, were measured. The authigenic Ba (Ba ex) contents were calculated and compared with the opal. The correlation coefficient between Ba ex and opal was quite small (r = 0.34), but it greatly grew larger (r = 0.90), if the Ba ex contents were multiplied by a simple function increasing with depth, except for two intervals. This may be due to the gradual change in the sedimentation environment during the glacial ages. One of the exceptional interval is found at 60–170 cm in depth, corresponding to 10–17 calendar kyr ago, the last termination period of glacial ages, where the Ba ex began to increase prior to opal. Since the calcium carbonate contents similarly increased prior to the opal increase, the Ba ex may be also related to calcareous organisms besides siliceous ones. The other is the last interglacial period around 120 kyr ago when the opal contents were high, but those of the Ba ex were not increased. This can be explained, if the Ba ex was reduced to sulfide and dissolved away in a strongly anoxic environment during the biologically productive period. During the glacial ages, the mass accumulation rate (MAR) of lithogenic Ti was about twice the amount of that during the interglacial ages. For opal, however, the contrast between the glacial and interglacial ages was more remarkable in its MAR than in its concentration in sediments, due to the larger variation in the bulk sedimentation rates.