84 citations as recorded by crossref.

1. Multiproxy record of suborbital-scale climate changes in the Algero-Balearic Basin during late MIS 20 - Termination IX O. Quivelli et al. 10.1016/j.quascirev.2021.106916
2. Response of macrobenthic and foraminifer communities to changes in deep-sea environmental conditions from Marine Isotope Stage (MIS) 12 to 11 at the “Shackleton Site” F. Rodríguez-Tovar et al. 10.1016/j.gloplacha.2015.08.012
3. Insolation forcing of coccolithophore productivity in the North Atlantic during the Middle Pleistocene C. Cavaleiro et al. 10.1016/j.quascirev.2018.05.027
4. 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
5. 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
6. Northern Mediterranean climate since the Middle Pleistocene: a 637 ka stable isotope record from Lake Ohrid (Albania/Macedonia) J. Lacey et al. 10.5194/bg-13-1801-2016
7. Combination of insolation and ice-sheet forcing drive enhanced humidity in northern subtropical regions during MIS 13 D. Oliveira et al. 10.1016/j.quascirev.2020.106573
8. Marine Isotope Stage 11: Palaeoclimates, palaeoenvironments and its role as an analogue for the current interglacial I. Candy et al. 10.1016/j.earscirev.2013.09.006
9. Oceanic heat pulses fueling moisture transport towards continental Europe across the mid-Pleistocene transition A. Bahr et al. 10.1016/j.quascirev.2017.11.009
10. Two-Tiered Transition of the North Atlantic Surface Hydrology during the Past 1.6 Ma: Multiproxy Evidence from Planktic Foraminifera M. Yamasaki et al. 10.2517/2020PR026
11. Re-evaluation of the “elevated epifauna” as indicator of Mediterranean Outflow Water in the Gulf of Cadiz using stable isotopes (δ 13 C, δ 18 O) Á. García-Gallardo et al. 10.1016/j.gloplacha.2017.06.005
12. Subtropical hydroclimate during Termination V (∼430-422 ka): Annual records of extreme precipitation, drought, and interannual variability from Santa Barbara Basin T. Napier et al. 10.1016/j.quascirev.2018.05.003
13. Spatial geochemistry of Upper Jurassic marine carbonates (Iberian subplate) R. Coimbra et al. 10.1016/j.earscirev.2014.08.011
14. Exceptional Agulhas leakage prolonged interglacial warmth during MIS 11c in Europe A. Koutsodendris et al. 10.1002/2014PA002665
15. The Marine Isotope Stage 12 pollen record from Lake Ohrid (SE Europe): Investigating short-term climate change under extreme glacial conditions A. Koutsodendris et al. 10.1016/j.quascirev.2019.105873
16. The environmental and evolutionary history of Lake Ohrid (FYROM/Albania): interim results from the SCOPSCO deep drilling project B. Wagner et al. 10.5194/bg-14-2033-2017
17. New bracketing luminescence ages constrain the Sima de los Huesos hominin fossils (Atapuerca, Spain) to MIS 12 M. Demuro et al. 10.1016/j.jhevol.2018.12.003
18. MIS 13-12 in Britain and the North Atlantic: understanding the palaeoclimatic context of the earliest Acheulean I. Candy et al. 10.1002/jqs.2816
19. Insights into North Atlantic deep water formation during the peak interglacial interval of Marine Isotope Stage 9 (MIS 9) Z. Mokeddem & J. McManus 10.1007/s00382-016-3505-9
20. High-latitude environmental change during MIS 9 and 11: biogeochemical evidence from Lake El'gygytgyn, Far East Russia R. D'Anjou et al. 10.5194/cp-9-567-2013
21. 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
22. The climate and vegetation of Marine Isotope Stage 11 – Model results and proxy-based reconstructions at global and regional scale T. Kleinen et al. 10.1016/j.quaint.2013.12.028
23. Carbon 13 Isotopes Reveal Limited Ocean Circulation Changes Between Interglacials of the Last 800 ka N. Bouttes et al. 10.1029/2019PA003776
24. A 1-Ma record of sea surface temperature and extreme cooling events in the North Atlantic: A perspective from the Iberian Margin T. Rodrigues et al. 10.1016/j.quascirev.2017.07.004
25. The cryptotephra record of the Marine Isotope Stage 12 to 10 interval (460–335 ka) at Tenaghi Philippon, Greece: Exploring chronological markers for the Middle Pleistocene of the Mediterranean region P. Vakhrameeva et al. 10.1016/j.quascirev.2018.09.019
26. Central Mediterranean Mid-Pleistocene paleoclimatic variability and its association with global climate L. Capotondi et al. 10.1016/j.palaeo.2015.11.009
27. Age and significance of the Quaternary cemented deposits of the Duje Valley (Picos de Europa, Northern Spain) E. Villa et al. 10.1016/j.yqres.2012.10.005
28. Change in the North Atlantic circulation associated with the mid-Pleistocene transition G. Martin-Garcia et al. 10.5194/cp-14-1639-2018
29. Palaeoceanographic changes in the North Atlantic during the Mid-Pleistocene Transition (MIS 31-19) as inferred from planktonic foraminiferal and calcium carbonate records I. Hernández-Almeida et al. 10.1111/j.1502-3885.2012.00283.x
30. Geomorphological and sedimentary processes of the glacially influenced northwestern Iberian continental margin and abyssal plains E. Llave et al. 10.1016/j.geomorph.2018.03.022
31. Abrupt variability of the last 24 ka BP recorded by coccolithophore assemblages off the Iberian Margin (core MD03-2699) E. PALUMBO et al. 10.1002/jqs.2623
32. Global and regional sea surface temperature trends during Marine Isotope Stage 11 Y. Milker et al. 10.5194/cp-9-2231-2013
33. Testing the extraction of past seawater Nd isotopic composition from North Atlantic deep sea sediments and foraminifera A. Elmore et al. 10.1029/2011GC003741
34. Response of the North Atlantic surface and intermediate ocean structure to climate warming of MIS 11 E. Kandiano et al. 10.1038/srep46192
35. Coccolithophores as proxy of seawater changes at orbital-to-millennial scale during middle Pleistocene Marine Isotope Stages 14-9 in North Atlantic core MD01-2446 M. Marino et al. 10.1002/2013PA002574
36. Oceanic Impact on European Climate Changes during the Quaternary G. Martin-Garcia 10.3390/geosciences9030119
37. Coccolithophore variability from the Shackleton Site (IODP Site U1385) through MIS 16-10 P. Maiorano et al. 10.1016/j.gloplacha.2015.07.009
38. Centennial-scale vegetation dynamics and climate variability in SE Europe during Marine Isotope Stage 11 based on a pollen record from Lake Ohrid I. Kousis et al. 10.1016/j.quascirev.2018.04.014
39. Forcing of late Pleistocene ice volume by spatially variable summer energy K. Haaga et al. 10.1038/s41598-018-29916-3
40. The continental record of Marine Isotope Stage 11 (Middle Pleistocene) on the Iberian Peninsula characterized by herpetofaunal assemblages H. Blain et al. 10.1002/jqs.2799
41. 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
42. Cold Water in a Warm World: Investigating the Origin of the Nordic Seas' Unique Surface Properties During MIS 11 J. Doherty & B. Thibodeau 10.3389/fmars.2018.00251
43. Subsurface North Atlantic warming as a trigger of rapid cooling events: evidence from the early Pleistocene (MIS 31–19) I. Hernández-Almeida et al. 10.5194/cp-11-687-2015
44. Source-to-sink pathways of clay minerals in the cadiz contourite system over the last 25 kyrs: The segregational role of mediterranean outflow water P. Moal-Darrigade et al. 10.1016/j.margeo.2021.106697
45. Towards a Middle Pleistocene terrestrial climate reconstruction based on herpetofaunal assemblages from the Iberian Peninsula: State of the art and perspectives H. Blain et al. 10.1016/j.quascirev.2018.04.019
46. Timing and cause of the disappearance of some elongated taxa in the Indian Ocean: Study from NGHP Hole 17A S. Biswas & A. Bhaumik 10.1007/s12040-020-01399-9
47. Dansgaard-Oeschger forcing of sea surface temperature variability in the midlatitude North Atlantic between 500 and 400 ka (MIS 12) B. Naafs et al. 10.1002/2014PA002697
48. Intermediate water variability of the subtropical Northeastern Atlantic during 490–424 ka (late MIS 13 and MIS 12) Q. Guo & B. Li 10.1016/j.margeo.2022.106730
49. Iron mineralogical proxies and Quaternary climate change in SE-European loess–paleosol sequences B. Buggle et al. 10.1016/j.catena.2013.06.012
50. A Middle Pleistocene Northeast Atlantic coccolithophore record: Paleoclimatology and paleoproductivity aspects F. Amore et al. 10.1016/j.marmicro.2012.03.006
51. Climate variability during MIS 20–18 as recorded by alkenone-SST and calcareous plankton in the Ionian Basin (central Mediterranean) M. Marino et al. 10.1016/j.palaeo.2020.110027
52. A stalagmite test of North Atlantic SST and Iberian hydroclimate linkages over the last two glacial cycles R. Denniston et al. 10.5194/cp-14-1893-2018
53. 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
54. Paleoceanography of the Bering Sea advanced by IODP Expedition 323: H. Asahi et al. 10.5575/geosoc.2017.0066
55. Sea-surface dynamics and palaeoenvironmental changes in the North Atlantic Ocean (IODP Site U1313) during Marine Isotope Stage 19 inferred from coccolithophore assemblages D. Emanuele et al. 10.1016/j.palaeo.2015.04.014
56. 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
57. Benthic foraminiferal response to orbital-scale variability in primary productivity off the Portuguese margin over the last 1.3 Myr Q. Guo et al. 10.1016/j.palaeo.2021.110532
58. Surface-ocean dynamics during eccentricity minima: a comparison between interglacial Marine Isotope Stage (MIS) 1 and MIS 11 on the Iberian Margin E. Palumbo et al. 10.1016/j.gloplacha.2018.10.011
59. Millennial scale coccolithophore paleoproductivity and surface water changes between 445 and 360ka (Marine Isotope Stages 12/11) in the Northeast Atlantic E. Palumbo et al. 10.1016/j.palaeo.2013.04.024
60. A paleoecological and paleobiogeographic evaluation of Helicosphaera inversa (Gartner) Theodoridis and the diachrony of its First Occurrence P. Maiorano et al. 10.1016/j.marmicro.2013.08.001
61. Climate and environments during Marine Isotope Stage 11 in the central Iberian Peninsula: the herpetofaunal assemblage from the Acheulean site of Áridos-1, Madrid H. Blain et al. 10.1016/j.quascirev.2014.04.009
62. The “MIS 11 paradox” and ocean circulation: Role of millennial scale events N. Vázquez Riveiros et al. 10.1016/j.epsl.2013.03.036
63. Bering Sea surface water conditions during Marine Isotope Stages 12 to 10 at Navarin Canyon (IODP Site U1345) B. Caissie et al. 10.5194/cp-12-1739-2016
64. Anomalous SST warming during MIS 13 in the Gulf of Lions (northwestern Mediterranean Sea) A. Cortina et al. 10.1016/j.orggeochem.2015.12.004
65. Chemical weathering of palaeosols from the Lower Palaeolithic site of Valle Giumentina, central Italy J. Degeai et al. 10.1016/j.quascirev.2018.01.014
66. Interglacial Paleoclimate in the Arctic T. Cronin et al. 10.1029/2019PA003708
67. Control Mechanisms of Primary Productivity Revealed by Calcareous Nannoplankton From Marine Isotope Stages 12 to 9 at the Shackleton Site (IODP Site U1385) A. González‐Lanchas et al. 10.1029/2021PA004246
68. 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
69. Potential CO2 forcing and Asian summer monsoon precipitation trends during the last 2,000 years W. Ren et al. 10.1515/geo-2020-0307
70. 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
71. 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
72. Suborbital-scale surface and deep water records in the subtropical North Atlantic: implications on thermohaline overturn K. Billups et al. 10.1016/j.quascirev.2011.06.015
73. Calcareous plankton response to orbital and millennial-scale climate changes across the Middle Pleistocene in the western Mediterranean A. Girone et al. 10.1016/j.palaeo.2013.09.005
74. The meridional temperature gradient in the eastern North Atlantic during MIS 11 and its link to the ocean–atmosphere system E. Kandiano et al. 10.1016/j.palaeo.2012.03.005
75. The Réunion Subchron vegetation and climate history of the northeastern Russian Arctic inferred from the Lake El'gygytgyn pollen record W. Zhao et al. 10.1016/j.palaeo.2015.06.047
76. Meltwater flux from northern ice-sheets to the mediterranean during MIS 12 L. Azibeiro et al. 10.1016/j.quascirev.2021.107108
77. A short-term climate oscillation during the Holsteinian interglacial (MIS 11c): An analogy to the 8.2ka climatic event? A. Koutsodendris et al. 10.1016/j.gloplacha.2012.05.011
78. The Marine Isotope Stage 19 in the mid-latitude North Atlantic Ocean: astronomical signature and intra-interglacial variability P. Ferretti et al. 10.1016/j.quascirev.2014.10.024
79. The Early and early Middle Pleistocene context of human occupation and lowland glaciation in Britain and northern Europe R. Preece & S. Parfitt 10.1016/j.quaint.2012.04.018
80. Millennial-scale ice rafting events and Hudson Strait Heinrich(-like) Events during the late Pliocene and Pleistocene: a review B. Naafs et al. 10.1016/j.quascirev.2013.08.014
81. The complexity of millennial-scale variability in southwestern Europe during MIS 11 D. Oliveira et al. 10.1016/j.yqres.2016.09.002
82. A new perspective of the Alboran Upwelling System reconstruction during the Marine Isotope Stage 11: A high-resolution coccolithophore record A. González-Lanchas et al. 10.1016/j.quascirev.2020.106520
83. Iberian Margin sea surface temperature during MIS 15 to 9 (580–300 ka): Glacial suborbital variability versus interglacial stability T. Rodrigues et al. 10.1029/2010PA001927
84. Calcareous plankton response to orbital and millennial-scale climate changes across the Middle Pleistocene in the western Mediterranean A. Girone et al. 10.1016/j.palaeo.2013.09.005