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Table 1 Results of paleomagnetic analysis

From: A centennial-resolution terrestrial climatostratigraphy and Matuyama–Brunhes transition record from a loess sequence in China

Depth Age T1 T2 No of steps MAD Dec Inc VGP lat. VGP lon.
(cm) (ka) (°C) (°C)    (°) (°) (°) (°)
154.0 764.37 200 680 11 1.6 7.7 48.0 81.1 − 122.1
166.5 764.69 250 650 11 4.1 − 7.5 55.6 83.8 29.8
176.0 764.93 200 400 5 13.3 − 4.4 − 25.4 41.4 − 67.0
197.0 765.55 200 560 9 7.1 51.1 − 64.3 − 4.7 − 109.0
197.0 765.55 250 530 7 5.9 56.7 − 56.8 0.5 − 114.2
204.5 765.77 200 650 12 6.8 144.1 2.5 − 40.6 157.9
209.5 765.91 200 590 10 3.1 2.8 55.3 87.6 177.4
212.0 765.98 200 590 10 5.6 − 4.1 46.9 82.2 − 44.7
230.0 766.50 250 620 11 2.6 − 4.4 50.9 85.0 − 24.5
247.0 767.99 200 590 10 3.9 0.5 54.5 89.6 − 160.4
258.0 768.95 200 560 7 1.9 − 5.2 48.0 82.6 − 34.9
271.0 770.09 350 620 8 2.9 − 5.7 49.7 83.4 − 24.3
281.0 771.32 200 620 11 2.7 1.1 55.0 89.0 168.5
290.0 772.48 450 680 8 6.4 18.5 32.5 66.1 − 120.8
300.0 773.76 200 590 10 5.7 − 16.1 46.8 74.6 − 5.3
304.0 774.28 300 620 9 3.1 7.2 43.1 78.3 − 106.5
309.0 774.84 200 530 8 5.4 − 7.0 50.2 82.9 − 15.4
314.0 775.32 200 560 9 5.4 − 10.1 50.7 80.8 − 3.0
321.5 776.04 300 560 7 11.3 35.2 68.5 59.9 152.7
326.5 776.52 300 530 6 12.1 9.6 41.6 76.1 − 112.1
331.5 776.82 350 590 7 9.3 23.4 58.8 70.9 176.8
332.0 776.84 250 560 8 8.9 − 2.0 40.4 77.9 − 63.8
337.0 776.96 450 590 5 9.9 16.7 21.7 61.8 − 109.2
342.0 777.09 200 560 9 7.2 184.0 − 61.2 − 82.1 − 50.5
347.0 777.21 250 590 9 10.0 126.2 − 34.4 − 40.1 − 166.8
350.0 777.29 350 590 7 11.8 25.0 34.8 62.8 − 133.4
355.0 777.41 250 530 7 6.0 − 7.4 43.3 78.3 − 37.6
357.5 777.47 250 650 8 6.9 160.1 − 1.6 − 51.1 140.2
360.0 777.54 250 590 9 8.4 7.0 50.9 83.2 − 134.0
362.5 777.60 250 530 7 6.8 16.6 56.5 76.4 − 176.1
363.0 777.61 250 560 8 5.8 − 6.8 44.1 79.1 − 38.3
368.0 777.74 250 590 9 10.2 9.2 45.9 79.0 − 120.5
370.5 777.80 250 620 11 6.4 161.3 − 21.1 − 60.5 147.1
373.0 777.86 200 590 10 5.6 160.1 − 28.1 − 63.1 154.0
375.5 777.93 200 620 11 1.4 176.8 − 46.4 − 82.2 128.7
379.5 778.03 200 590 10 5.7 0.2 45.0 81.5 − 73.8
382.0 778.09 300 620 9 11.6 183.8 − 56.9 − 86.1 − 22.3
384.5 778.15 200 680 13 2.6 167.0 − 57.6 − 79.1 − 141.8
387.0 778.21 200 680 13 2.5 164.5 − 40.6 − 72.2 160.3
389.5 778.27 300 530 6 7.7 164.1 − 37.2 − 71.8 149.0
392.0 778.34 200 680 13 1.3 180.3 − 43.5 − 80.3 105.8
394.5 778.40 200 680 13 1.3 178.3 − 49.2 − 84.8 124.0
395.0 778.42 250 680 12 6.9 179.1 − 57.3 − 87.0 − 86.5
397.5 778.48 200 680 13 2.2 170.1 − 45.1 − 78.1 155.4
400.0 778.55 200 680 12 2.5 167.6 − 48.5 − 78.1 172.9
402.5 778.61 200 680 12 1.3 175.1 − 43.7 − 79.6 132.7
405.0 778.68 200 680 13 1.7 169.2 − 52.2 − 80.8 − 173.5
406.0 778.71 250 680 12 1.7 176.5 − 52.1 − 86.3 159.7
408.5 778.77 200 680 13 2.4 163.4 − 47.3 − 74.4 176.9
411.0 778.84 300 530 6 9.8 − 88.3 71.3 29.3 67.4
413.5 778.90 300 530 6 9.8 − 47.0 53.3 51.6 29.6
416.0 778.97 300 560 7 4.1 198.4 − 45.7 − 72.4 39.0
418.5 779.04 300 560 7 3.5 160.2 − 45.0 − 71.0 176.3
  1. T1, T2 Temperature ranges of thermal demagnetization data used for principal component analysis