Kuptsov, Vladimir M; Lisitzin, Alexander P; Zel'dina, Bella B (1982): (Table 2) Radiocarbon datings of bottom sediments from the Gulf of Riga, Baltic Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755602, Supplement to: Kuptsov, VM et al. (1982): Sedimentation rates in the Gulf of Riga, from radiocarbon data. Oceanology, 22(4), 455-458
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Published: 1982 (exact date unknown) • DOI registered: 2011-02-09
Abstract:
Radiocarbon datings have been made on bottom sediments collected in the Gulf of Riga. These age determinations have been made on organic matter, much of which supplied with stream runoff and having some initial ages ranging from 2000 to 6000 yrs (in different rivers). This greatly complicates interpretation of obtained data. Average sedimentation rates, as determined by the equation of linear regression for four sediment cores, vary from 0.2 to 2.0 mm/yr.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 57.370360 * Median Longitude: 23.750680 * South-bound Latitude: 57.096700 * West-bound Longitude: 23.140000 * North-bound Latitude: 57.700000 * East-bound Longitude: 24.265000
Minimum DEPTH, sediment/rock: 0.020 m * Maximum DEPTH, sediment/rock: 5.315 m
Event(s):
AK26A-2576 * Latitude: 57.096700 * Longitude: 23.970000 * Elevation: -21.0 m * Location: Gulf of Riga * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
AK26A-2579 * Latitude: 57.271700 * Longitude: 24.265000 * Elevation: -25.0 m * Location: Gulf of Riga * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
AK26A-2590 * Latitude: 57.201700 * Longitude: 23.786700 * Elevation: -42.0 m * Location: Gulf of Riga * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 6 | Depth, top/min | Depth top | m | Kuptsov, Vladimir M | ||
| 7 | Depth, bottom/max | Depth bot | m | Kuptsov, Vladimir M | ||
| 8 | Age, dated | Age dated | ka | Kuptsov, Vladimir M | Age, radiocarbon | |
| 9 | Age, dated, standard deviation | Age dated std dev | ± | Kuptsov, Vladimir M | Age, radiocarbon |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
123 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 Age dated [ka] | 9 Age dated std dev [±] |
|---|---|---|---|---|---|---|---|---|
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 0.020 | 0.00 | 0.04 | 5.72 | 0.15 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 0.140 | 0.12 | 0.16 | 11.64 | 0.39 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 0.800 | 0.75 | 0.85 | 9.15 | 0.16 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 1.100 | 1.05 | 1.15 | 10.09 | 0.19 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 1.550 | 1.50 | 1.60 | 9.95 | 0.17 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 2.050 | 2.00 | 2.10 | 10.65 | 0.19 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 2.650 | 2.60 | 2.70 | 10.65 | 0.89 |
| AK26A-2576 | 57.0967 | 23.9700 | -21 | 3.250 | 3.20 | 3.30 | 14.31 | 0.21 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 0.150 | 0.10 | 0.20 | 10.37 | 0.18 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 0.700 | 0.65 | 0.75 | 11.97 | 0.18 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 1.250 | 1.20 | 1.30 | 11.89 | 0.54 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 1.850 | 1.80 | 1.90 | 14.90 | 0.33 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 2.700 | 2.65 | 2.75 | 7.15 | |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 3.375 | 3.35 | 3.40 | 13.93 | 0.26 |
| AK26A-2579 | 57.2717 | 24.2650 | -25 | 4.050 | 4.00 | 4.10 | 11.56 | 0.48 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 0.150 | 0.10 | 0.20 | 1.58 | 0.14 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 0.250 | 0.20 | 0.30 | 2.19 | 0.22 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 0.750 | 0.70 | 0.80 | 5.42 | 0.17 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 1.350 | 1.30 | 1.40 | 7.60 | 0.15 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 1.750 | 1.70 | 1.80 | 10.15 | 0.22 |
| AK26A-2590 | 57.2017 | 23.7867 | -42 | 5.315 | 5.05 | 5.58 | 17.60 | 0.41 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 0.150 | 0.10 | 0.20 | 4.45 | 0.19 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 1.025 | 1.00 | 1.05 | 5.75 | 0.23 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 2.025 | 2.00 | 2.05 | 7.49 | 0.27 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 2.725 | 2.70 | 2.75 | 7.26 | 0.33 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 3.425 | 3.40 | 3.45 | 9.29 | 0.35 |
| AK26A-2593 | 57.5817 | 23.1400 | -42 | 4.125 | 4.10 | 4.15 | 12.70 | 0.49 |
| AK26A-2601 | 57.7000 | 23.5917 | -53 | 0.150 | 0.10 | 0.20 | 2.41 | 0.26 |
| AK26A-2601 | 57.7000 | 23.5917 | -53 | 1.050 | 1.00 | 1.10 | 2.72 | 0.18 |
| AK26A-2601 | 57.7000 | 23.5917 | -53 | 2.050 | 2.00 | 2.10 | 3.53 | 0.16 |
| AK26A-2601 | 57.7000 | 23.5917 | -53 | 3.050 | 3.00 | 3.10 | 3.77 | 0.12 |