Kravchinsky, Vadim; Langereis, Cornelis G; Walker, Shawn D; Dlusskiy, Konstantin G; White, Dustin (2013): Piecewise linear-interpolation of frequency dependence of magnetic susceptibility of soil/loess section Burdukovo [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.820131, In supplement to: Kravchinsky, V et al. (2013): Discovery of Holocene millennial climate cycles in the Asian continental interior: Has the sun been governing the continental climate? Global and Planetary Change, 110(C), 386-396, https://doi.org/10.1016/j.gloplacha.2013.02.011
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Latitude: 52.100000 * Longitude: 107.500000
Event(s):
Comment:
DEPTH, sediment/rock [m] is the composite depth of the section, AGE [ka BP] is the resampled and interpolated age. Integration interpolation: mean values between mid-points.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | AGE | Age | ka BP | Geocode | ||
| 2 | Factor | Factor | Kravchinsky, Vadim | interpolated | frequency dependence of magnetic susceptibility (FD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
189 data points
Data
| 1 Age [ka BP] | 2 Factor |
|---|---|
| 0.10 | 1.70 |
| 0.15 | 1.70 |
| 0.20 | 1.51 |
| 0.25 | 1.16 |
| 0.30 | 1.12 |
| 0.35 | 1.13 |
| 0.40 | 0.90 |
| 0.45 | 0.59 |
| 0.50 | 0.69 |
| 0.55 | 0.51 |
| 0.60 | 0.22 |
| 0.65 | 0.31 |
| 0.70 | 0.58 |
| 0.75 | 0.63 |
| 0.80 | 0.36 |
| 0.85 | 0.54 |
| 0.90 | 0.83 |
| 0.95 | 0.92 |
| 1.00 | 0.75 |
| 1.05 | 0.60 |
| 1.10 | 0.66 |
| 1.15 | 0.16 |
| 1.20 | 0.34 |
| 1.25 | 0.21 |
| 1.30 | 0.20 |
| 1.35 | 0.45 |
| 1.40 | 0.35 |
| 1.45 | 0.47 |
| 1.50 | 0.50 |
| 1.55 | 0.23 |
| 1.60 | 0.21 |
| 1.65 | 0.50 |
| 1.70 | 0.91 |
| 1.75 | 0.49 |
| 1.80 | 0.34 |
| 1.85 | 0.65 |
| 1.90 | 0.31 |
| 1.95 | 0.49 |
| 2.00 | 0.26 |
| 2.05 | 0.31 |
| 2.10 | 1.53 |
| 2.15 | 2.12 |
| 2.20 | 0.79 |
| 2.25 | 0.23 |
| 2.30 | 0.05 |
| 2.35 | 0.26 |
| 2.40 | 0.33 |
| 2.45 | 0.41 |
| 2.50 | 2.43 |
| 2.55 | 2.49 |
| 2.60 | 1.65 |
| 2.65 | 0.52 |
| 2.70 | 0.30 |
| 2.75 | 0.26 |
| 2.80 | 0.20 |
| 2.85 | 0.37 |
| 2.90 | 0.47 |
| 2.95 | 0.51 |
| 3.00 | 0.68 |
| 3.05 | 0.78 |
| 3.10 | 0.88 |
| 3.15 | 1.03 |
| 3.20 | 0.87 |
| 3.25 | 0.41 |
| 3.30 | 0.64 |
| 3.35 | 0.54 |
| 3.40 | 0.38 |
| 3.45 | 0.31 |
| 3.50 | 0.66 |
| 3.55 | 1.60 |
| 3.60 | 3.07 |
| 3.65 | 4.66 |
| 3.70 | 3.81 |
| 3.75 | 2.66 |
| 3.80 | 2.04 |
| 3.85 | 1.13 |
| 3.90 | 0.95 |
| 3.95 | 0.94 |
| 4.00 | 0.96 |
| 4.05 | 1.00 |
| 4.10 | 1.04 |
| 4.15 | 1.03 |
| 4.20 | 0.86 |
| 4.25 | 0.67 |
| 4.30 | 0.48 |
| 4.35 | 0.94 |
| 4.40 | 1.11 |
| 4.45 | 0.85 |
| 4.50 | 0.63 |
| 4.55 | 0.76 |
| 4.60 | 1.05 |
| 4.65 | 1.42 |
| 4.70 | 1.66 |
| 4.75 | 1.53 |
| 4.80 | 1.38 |
| 4.85 | 1.23 |
| 4.90 | 1.17 |
| 4.95 | 1.21 |
| 5.00 | 1.25 |
| 5.05 | 1.31 |
| 5.10 | 0.79 |
| 5.15 | 0.14 |
| 5.20 | 0.26 |
| 5.25 | 0.54 |
| 5.30 | 0.38 |
| 5.35 | 0.44 |
| 5.40 | 0.88 |
| 5.45 | 0.91 |
| 5.50 | 0.80 |
| 5.55 | 0.57 |
| 5.60 | 0.34 |
| 5.65 | 0.45 |
| 5.70 | 0.42 |
| 5.75 | 0.44 |
| 5.80 | 1.13 |
| 5.85 | 0.81 |
| 5.90 | 0.88 |
| 5.95 | 0.68 |
| 6.00 | 0.39 |
| 6.05 | 0.32 |
| 6.10 | 0.26 |
| 6.15 | 0.31 |
| 6.20 | 0.35 |
| 6.25 | 0.35 |
| 6.30 | 0.36 |
| 6.35 | 0.47 |
| 6.40 | 0.62 |
| 6.45 | 0.39 |
| 6.50 | 0.53 |
| 6.55 | 1.64 |
| 6.60 | 1.12 |
| 6.65 | 0.58 |
| 6.70 | 1.38 |
| 6.75 | 2.38 |
| 6.80 | 1.99 |
| 6.85 | 1.13 |
| 6.90 | 0.42 |
| 6.95 | 0.76 |
| 7.00 | 0.36 |
| 7.05 | 1.06 |
| 7.10 | 0.60 |
| 7.15 | 0.32 |
| 7.20 | 0.48 |
| 7.25 | 0.38 |
| 7.30 | 0.27 |
| 7.35 | 0.51 |
| 7.40 | 0.39 |
| 7.45 | 0.56 |
| 7.50 | 1.06 |
| 7.55 | 1.18 |
| 7.60 | 1.41 |
| 7.65 | 0.91 |
| 7.70 | 2.29 |
| 7.75 | 2.36 |
| 7.80 | 2.03 |
| 7.85 | 1.63 |
| 7.90 | 1.44 |
| 7.95 | 1.76 |
| 8.00 | 1.91 |
| 8.05 | 1.29 |
| 8.10 | 1.10 |
| 8.15 | 1.30 |
| 8.20 | 1.24 |
| 8.25 | 1.11 |
| 8.30 | 0.87 |
| 8.35 | 1.08 |
| 8.40 | 1.35 |
| 8.45 | 1.62 |
| 8.50 | 1.89 |
| 8.55 | 1.93 |
| 8.60 | 1.77 |
| 8.65 | 1.79 |
| 8.70 | 2.02 |
| 8.75 | 1.92 |
| 8.80 | 1.63 |
| 8.85 | 1.56 |
| 8.90 | 1.54 |
| 8.95 | 1.05 |
| 9.00 | 0.82 |
| 9.05 | 1.25 |
| 9.10 | 2.37 |
| 9.15 | 2.02 |
| 9.20 | 1.46 |
| 9.25 | 1.10 |
| 9.30 | 0.92 |
| 9.35 | 0.54 |
| 9.40 | 0.65 |
| 9.45 | 1.03 |
| 9.50 | 0.31 |