25 citations as recorded by crossref.

1. Machine learning approach reveals strong link between obliquity amplitude increase and the Mid-Brunhes transition T. Mitsui & N. Boers
2. The deterministic excitation paradigm and the late Pleistocene glacial terminations S. Pierini
3. The middle Pleistocene transition by frequency locking and slow ramping of internal period K. Nyman & P. Ditlevsen
4. Is there 1.5-million-year-old ice near Dome C, Antarctica? F. Parrenin et al.
5. Simulating global ice volume across the Mid-Pleistocene Transition with a ramp-like increase in the deglaciation threshold F. Pollak et al.
6. Orbital insolation variations, intrinsic climate variability, and Quaternary glaciations K. Riechers et al.
7. Distinct roles for precession, obliquity, and eccentricity in Pleistocene 100-kyr glacial cycles S. Barker et al.
8. Insolation evolution and ice volume legacies determine interglacial and glacial intensity T. Mitsui et al.
9. Why could ice ages be unpredictable? M. Crucifix
10. Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al.
11. Synchronization phenomena observed in glacial–interglacial cycles simulated in an Earth system model of intermediate complexity T. Mitsui et al.
12. Unusual weakening trend of the East Asian winter monsoon during MIS 8 revealed by Chinese loess deposits and its implications for ice age dynamics Q. Hao et al.
13. Obliquity and precession as pacemakers of Pleistocene deglaciations F. Feng & C. Bailer-Jones
14. A gradual change is more likely to have caused the Mid-Pleistocene Transition than an abrupt event E. Legrain et al.
15. ZEMBA v1.0: an energy and moisture balance climate model to investigate Quaternary climate D. Gunning et al.
16. Influence of the choice of insolation forcing on the results of a conceptual glacial cycle model G. Leloup & D. Paillard
17. The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record W. Zhao et al.
18. A simple rule to determine which insolation cycles lead to interglacials P. Tzedakis et al.
19. Pronounced northward shift of the westerlies during MIS 17 leading to the strong 100-kyr ice age cycles M. Sánchez Goñi et al.
20. Interglacials of the last 800,000 years
21. 100 kyr ice age cycles as a timescale-matching problem T. Mitsui et al.
22. Species composition and mtDNA diversity of small mammals in the northern and central parts of Japan shaped by Quaternary environmental fluctuations H. Suzuki & S. Ohdachi
23. Late Pleistocene 100-kyr glacial cycles paced by precession forcing of summer insolation B. Hobart et al.
24. Regional and global benthic δ18O stacks for the last glacial cycle L. Lisiecki & J. Stern
25. Quaternary glaciations: from observations to theories D. Paillard