14 citations as recorded by crossref.

1. A molecular isotope record of climate variability and vegetation response in southwestern North America during mid-Pleistocene glacial/interglacial cycles S. Contreras et al. 10.1016/j.palaeo.2016.07.019
2. A modified seasonal cycle during MIS31 super-interglacial favors stronger interannual ENSO and monsoon variability F. Justino et al. 10.5194/cp-15-735-2019
3. Impact processes, permafrost dynamics, and climate and environmental variability in the terrestrial Arctic as inferred from the unique 3.6 Myr record of Lake El'gygytgyn, Far East Russia – A review V. Wennrich et al. 10.1016/j.quascirev.2016.03.019
4. Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
5. Oceanic response to changes in the WAIS and astronomical forcing during the MIS31 superinterglacial F. Justino et al. 10.5194/cp-13-1081-2017
6. Changes in temperature and oxygen isotopic composition of Mediterranean water during the Mid-Pleistocene transition in the Montalbano Jonico section (southern Italy) using the clumped-isotope thermometer M. Peral et al. 10.1016/j.palaeo.2020.109603
7. Diverse response of global terrestrial vegetation to astronomical forcing and CO2 during the MIS-11 and MIS-13 interglacials Q. Su et al. 10.1007/s00382-022-06308-y
8. Southern hemisphere monsoonal system during superinterglacial stages: MIS5e, MIS11c and MIS31 C. de Sousa Gurjão et al. 10.1007/s00382-023-06660-7
9. Southern ocean response to glacial and interglacial forcing N. Leonardo et al. 10.1016/j.jsames.2023.104642
10. Summer warmth of the past six interglacials on Greenland A. Cluett & E. Thomas 10.1073/pnas.2022916118
11. Unexpected weak seasonal climate in the western Mediterranean region during MIS 31, a high-insolation forced interglacial D. Oliveira et al. 10.1016/j.quascirev.2017.02.013
12. Controls on Terrigenous Detritus Deposition and Oceanography Changes in the Central Okhotsk Sea Over the Past 1550 ka Y. Chou et al. 10.3389/feart.2021.683984
13. Climate response to drastically modified PDO, PNA and NAM in the superinterglacial MIS 31 F. Justino et al. 10.1111/bor.12556
14. Sea-level rise due to polar ice-sheet mass loss during past warm periods A. Dutton et al. 10.1126/science.aaa4019