Table 1 Comparison of multiple frequency (decadal- to millennial-scale) periodicities identified in the geological records.
Record | Age | Decadal- to centennial-scale periodicities (year cycle) | References | ||||||
|---|---|---|---|---|---|---|---|---|---|
Total solar irradiance (TSI), 14C, 10Be | Holocene | 10.9 Schwabe | 88–120 Gleissberg | 208 de Vries | – | 350 | 506 | 710 | |
Hulu Cave and GRIP d18O | Late Pleistocene | – | – | – | 286 | 352 | 512 | 712 | Clemens64 |
Antarctic ice-core EDC δ18O | Middle–Late Pleistocene | – | – | – | – | – | – | – | Calculated by this study; data from Barker et al.7 |
Lacustrine deposits Ostracod, GR, MS | Late Miocene | – | 110–123 | 209 | – | 352 | 510 | – | |
Lacustrine varve | Middle Eocene | 10–11 | 70–90 | – | – | – | – | – | Shi et al.20 |
Lacustrine varve Pollen | Early Eocene | 10–11 | 82 | 210–231 | – | 420–438 | – | – | |
Marine marlstone XRF core scanner | early Late Cretaceous (mid-Cenomanian) | – | 80–100 | 200–230 | – | 393–412 | 569 | – | Ma et al.21 |
Marine deposits benthic Foraminifera | late Early Cretaceous (Albian OAE1b) | – | – | – | – | – | ~ 500 | – | Friedrich et al.32 |
Lacustrine varve, XRF core scanner, Ca/Ti variations | late Early Cretaceous (Barremian–Aptian) | 11.4 | 84–125 | 185–212 | 263–284 | 361–412 | 524–568 | 686–716 | This study |
Marine marl-limestone Rock magnetic | Late Jurassic | – | – | – | – | – | – | – | Boulila et al.22 |
Rock magnetic | Early Triassic | – | – | – | – | – | – | – | Wu et al.60 |
Rhythmite | Late Carboniferous–Early Permian | – | – | – | – | – | – | – | Franco et al.59 |
Ti variations | Early Devonian | – | – | – | – | – | – | – | da Silva et al.61 |
Record | Age | Millennial-scale Periodicities (kyr cycle) | References | ||||||
|---|---|---|---|---|---|---|---|---|---|
Total solar irradiance (TSI), 14C, 10Be | Holocene | 0.9–1.2 Eddy | – | 2.0–2.5 Hallstatt | – | 5.0 | – | – | |
Hulu Cave and GRIP d18O | Late Pleistocene | 1.1–1.3 | 1.5–1.7 | 2.0–2.2 | 3.0 | 4.0–4.8 | – | 10.0 | Clemens64 |
Antarctic ice-core EDC δ18O | Middle–Late Pleistocene | – | 1.5 | 2.0–2.5 | 3.1–3.7 | 4.5–5.5 | 7.0–7.4 | 10.0–11.0 | Calculated by this study; data from Barker et al.7 |
Lacustrine deposits Ostracod, GR, MS | Late Miocene | 1.0 | – | 2.3 | – | – | – | – | |
Lacustrine varve | Middle Eocene | – | – | – | – | – | – | – | Shi et al.20 |
Lacustrine varve Pollen | Early Eocene | 0.9 | 1.6–1.7 | 2.3–2.4 | 3.6–3.7 | – | 7.4–7.6 | – | |
Marine marlstone XRF core scanner | early Late Cretaceous (mid-Cenomanian) | – | 1.6–1.7 | – | – | ~ 4.8 | – | – | Ma et al.21 |
Marine deposits Benthic Foraminifera | late Early Cretaceous (Albian OAE1b) | 1.25 | – | – | – | 5.7 | – | – | Friedrich et al.32 |
Lacustrine varve, XRF core scanner, Ca/Ti variations | late Early Cretaceous (Barremian–Aptian) | 1.0–1.25 | 1.4–1.5 | 1.8–2.1 | 3.2–3.9 | 4.6–5.6 | ~ 7.3 | 10.0–12.0 | This study |
Marine marl-limestone Rock magnetic | Late Jurassic | – | 1.35–1.54 | – | – | 5.2 | – | 10.5 | Boulila et al.22 |
Rock magnetic | Early Triassic | – | – | – | 3.8 | 4.7–5.3 | 6.8 | 11.0 | Wu et al.60 |
Rhythmite | Late Carboniferous–Early Permian | – | – | 2.0–2.5 | 3.5–3.6 | 4.0–5.4 | – | 11.1–13.6 | Franco et al.59 |
Ti variations | Early Devonian | 0.8–1.1 | – | 2.5 | – | – | 6.0–7.0 | 10.0–12.0 | da Silva et al.61 |