62 citations as recorded by crossref.

1. The Fucino 250–170 ka tephra record: New insights on peri-Tyrrhenian explosive volcanism, central mediterranean tephrochronology, and timing of the MIS 8-6 climate variability L. Monaco et al. 10.1016/j.quascirev.2022.107797
2. Solar activity, cosmic rays, and earth temperature reconstructions for the past two millennia. Part 2. Analysis of the relation between the global temperature variations and natural processes V. Dergachev 10.1134/S0016793215020036
3. Strong and deep Atlantic meridional overturning circulation during the last glacial cycle E. Böhm et al. 10.1038/nature14059
4. Relative sea-level variability during the late Middle Pleistocene: New evidence from eastern England N. Barlow et al. 10.1016/j.quascirev.2017.08.017
5. An optimized scheme of lettered marine isotope substages for the last 1.0 million years, and the climatostratigraphic nature of isotope stages and substages L. Railsback et al. 10.1016/j.quascirev.2015.01.012
6. Planktonic foraminifera response to orbital and millennial-scale climate variability at the southern Iberian Margin (IODP Site U1385) during Marine Isotope Stages 20 and 19 A. Girone et al. 10.1016/j.palaeo.2023.111450
7. Emergence of regional cultural traditions during the Lower Palaeolithic: the case of Frosinone-Ceprano basin (Central Italy) at the MIS 11–10 transition M. Moncel et al. 10.1007/s12520-020-01150-x
8. Coccolithophore productivity at the western Iberian Margin during the Middle Pleistocene (310–455 ka) – evidence from coccolith Sr∕Ca data C. Cavaleiro et al. 10.5194/cp-16-2017-2020
9. Increase in the global climate variability from about 400 ka BP until present N. Vakulenko et al. 10.1134/S1028334X14060300
10. Meltwater flux from northern ice-sheets to the mediterranean during MIS 12 L. Azibeiro et al. 10.1016/j.quascirev.2021.107108
11. Tropical Atlantic Cooling and Freshening in the Middle of the Last Interglacial From Coral Proxy Records W. Brocas et al. 10.1029/2019GL083094
12. Cosmogenic nuclides constrain surface fluctuations of an East Antarctic outlet glacier since the Pliocene R. Jones et al. 10.1016/j.epsl.2017.09.014
13. Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
14. Review of the Early–Middle Pleistocene boundary and Marine Isotope Stage 19 M. Head 10.1186/s40645-021-00439-2
15. Atmospheric CO2 forcing on Mediterranean biomes during the past 500 kyrs A. Koutsodendris et al. 10.1038/s41467-023-37388-x
16. Problem of the length of the current interglacial V. Dergachev & O. Raspopov 10.1134/S0016793213070049
17. Marine and terrestrial climate variability in the western Mediterranean Sea during marine isotope stages 20 and 19 F. Toti et al. 10.1016/j.quascirev.2020.106486
18. A Dynamic, Coupled Thermal Reservoir Approach to Atmospheric Energy Transfer Part I: Concepts R. Clark 10.1260/0958-305X.24.3-4.319
19. Sequence of events from the onset to the demise of the Last Interglacial: Evaluating strengths and limitations of chronologies used in climatic archives A. Govin et al. 10.1016/j.quascirev.2015.09.018
20. Persistent influence of precession on northern ice sheet variability since the early Pleistocene S. Barker et al. 10.1126/science.abm4033
21. Understanding glacial cycles: A multivariate disequilibrium approach R. Kaufmann & F. Pretis 10.1016/j.quascirev.2020.106694
22. Similarities among glacials and interglacials in the LR04 benthic oxygen isotope stack over the last 1.014 million years revealed by cluster analysis and a DTW algorithm D. Wieczorek et al. 10.1016/j.gloplacha.2021.103521
23. Climate archives from 90 to 250 ka in horizontal and vertical ice cores from the Allan Hills Blue Ice Area, Antarctica N. Spaulding et al. 10.1016/j.yqres.2013.07.004
24. Interglacials of the last 800,000 years 10.1002/2015RG000482
25. Palaeobiogeography of NE Atlantic archipelagos during the last Interglacial (MIS 5e): A molluscan approach to the conundrum of Macaronesia as a marine biogeographic unit C. Melo et al. 10.1016/j.quascirev.2023.108313
26. Reconstruction of surface water dynamics in the North Atlantic during the Mid-Pleistocene (~540–400 ka), as inferred from coccolithophores and planktonic foraminifera M. Martínez-Sánchez et al. 10.1016/j.marmicro.2019.03.002
27. Response of the North Atlantic surface and intermediate ocean structure to climate warming of MIS 11 E. Kandiano et al. 10.1038/srep46192
28. MOW strengthening and contourite development over two analog climate cycles (MIS 12–11 and MIS 2–1) in the Gulf of Cadíz: An impact on North Atlantic climate during deglaciation V and MIS 11? P. Moal-Darrigade et al. 10.1016/j.gloplacha.2021.103721
29. Climatic stages recorded in sediments of the Gunang Cave, South Korea J. Kim et al. 10.1016/j.quaint.2013.05.013
30. 40Ar/39Ar geochronologic and paleoenvironmental constraints to glacial termination III and MIS 7e, 7c, and 7a sea level fluctuations on the Tyrrhenian Sea coast of Italy F. Bulian et al. 10.1016/j.gloplacha.2024.104594
31. A 600,000 year long continental pollen record from Lake Van, eastern Anatolia (Turkey) T. Litt et al. 10.1016/j.quascirev.2014.03.017
32. Terminations VI and VIII (∼ 530 and ∼ 720 kyr BP) tell us the importance of obliquity and precession in the triggering of deglaciations F. Parrenin & D. Paillard 10.5194/cp-8-2031-2012
33. The response of the Bering Sea Gateway during the Mid-Pleistocene Transition Z. Stroynowski et al. 10.1016/j.palaeo.2017.08.023
34. Evidence for regional cooling, frontal advances, and East Greenland Ice Sheet changes during the demise of the last interglacial N. Irvalı et al. 10.1016/j.quascirev.2016.08.029
35. A multi-proxy record of MIS 11–12 deglaciation and glacial MIS 12 instability from the Sulmona basin (central Italy) E. Regattieri et al. 10.1016/j.quascirev.2015.11.015
36. Exceptional Agulhas leakage prolonged interglacial warmth during MIS 11c in Europe A. Koutsodendris et al. 10.1002/2014PA002665
37. Sensitivity of the Antarctic ice sheets to the warming of marine isotope substage 11c M. Mas e Braga et al. 10.5194/tc-15-459-2021
38. The structure of marine isotope Stage 11 and its alignment with the Holocene Y. Wang et al. 10.1016/j.palaeo.2022.111311
39. A 1.5-million-year record of orbital and millennial climate variability in the North Atlantic D. Hodell et al. 10.5194/cp-19-607-2023
40. Mediterranean Outflow and surface water variability off southern Portugal during the early Pleistocene: A snapshot at Marine Isotope Stages 29 to 34 (1020–1135 ka) A. Voelker et al. 10.1016/j.gloplacha.2015.08.015
41. Calcareous plankton and the mid-Brunhes climate variability in the Alboran Sea (ODP Site 977) M. Marino et al. 10.1016/j.palaeo.2018.07.023
42. Climate signatures through Marine Isotope Stage 19 in the Montalbano Jonico section (Southern Italy): A land–sea perspective P. Maiorano et al. 10.1016/j.palaeo.2016.08.029
43. Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays H. Kajita et al. 10.1186/s40645-022-00499-y
44. Pastoralism may have delayed the end of the green Sahara C. Brierley et al. 10.1038/s41467-018-06321-y
45. Ice Sheets and the Anthropocene E. Wolff 10.1144/SP395.10
46. Early Interglacial Legacy of Deglacial Climate Instability S. Barker et al. 10.1029/2019PA003661
47. Astronomical forcing shaped the timing of early Pleistocene glacial cycles Y. Watanabe et al. 10.1038/s43247-023-00765-x
48. Saharan dust deposition in the Carpathian Basin and its possible effects on interglacial soil formation G. Varga et al. 10.1016/j.aeolia.2016.05.004
49. The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 L. Menviel et al. 10.5194/gmd-12-3649-2019
50. Reorganization of Atlantic Waters at sub-polar latitudes linked to deep-water overflow in both glacial and interglacial climate states D. Holmes et al. 10.5194/cp-18-989-2022
51. Comparative carbon cycle dynamics of the present and last interglacial V. Brovkin et al. 10.1016/j.quascirev.2016.01.028
52. Climate‐driven ecological stability as a globally shared cause of Late Quaternary megafaunal extinctions: the Plaids and Stripes Hypothesis D. Mann et al. 10.1111/brv.12456
53. Duration and dynamics of the best orbital analogue to the present interglacial B. Giaccio et al. 10.1130/G36677.1
54. A simple rule to determine which insolation cycles lead to interglacials P. Tzedakis et al. 10.1038/nature21364
55. Abrupt CO 2 release to the atmosphere under glacial and early interglacial climate conditions C. Nehrbass-Ahles et al. 10.1126/science.aay8178
56. Sea surface water variability during the Mid-Brunhes inferred from calcareous plankton in the western Mediterranean (ODP Site 975) P. Maiorano et al. 10.1016/j.palaeo.2016.07.006
57. Ocean-atmosphere interconnections from the last interglacial to the early glacial: An integration of marine and cave records in the Iberian region J. Torner et al. 10.1016/j.quascirev.2019.106037
58. Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic Z. Mokeddem et al. 10.1073/pnas.1322103111
59. 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
60. Pleistocene–Holocene climatic events on the inner coastal plain of southernmost Brazil in relation to marine isotopic stages V. Ribeiro et al. 10.1016/j.jsames.2024.104857
61. A reference time scale for Site U1385 (Shackleton Site) on the SW Iberian Margin D. Hodell et al. 10.1016/j.gloplacha.2015.07.002
62. Historic Variability: Informing Restoration Strategies, Not Prescribing Targets C. Millar 10.1080/10549811.2014.887474