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. 2019 Mar 4;116(22):10664–10673. doi: 10.1073/pnas.1813901116

Table 2.

Periods of the different arguments in the Newark–Hartford data using MTM analysis, FA, and corresponding values in the FA of the La2010d* and La2010a solutions (5) for Earth’s eccentricity (SI Appendix, Table S4)

Row Argument (frequency) MTM period (ky) FA period (ky) La2010d* period (ky) La2010a§ period (ky)
1 g4 − g3 1,724.63 1,747.65 1,793.04 2,368.95
2 g1 − g5 923.04 923.16 957.56 967.42
3 g2 − g1 720.18 719.05 704.98 697.63
4 (g2 − g5) − (g4 − g3) 537.18 527.56 515.09 489.37
5 g2 − g5 405.17 404.97 404.58 405.63
6 (g2 − g5) + (g4 − g3) 336.53 335.13 330.08 346.42
7 g3 − g2 132.53 132.17 132.58 130.71
8 g4 − g2 122.96 123.08 123.47 123.88
9 g3 − g5 99.83 99.78 99.86 98.85
10 g4 − g5 94.43 94.49 94.62 94.89

All terms are recovered by FA in the 14 terms of larger amplitude (SI Appendix, Table S5), except g1 − g5 and g2 − g5 + (g4 − g3), which are of lower amplitude.

La2010d* is taken over the interval 209–231 Ma.

§

La2010a is taken over the interval 0–20 Ma.