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2921 Publications found! (Query time: 0.004 s) – Download as CSV file – Download as KML file

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ScoreExp/Site/HoleYear ↑Author/TitleFull text
25%199
199-1218
199-1219
320
320-U1334		2012Takata, Hiroyuki; Nomura, Ritsuo et al.: Late early Oligocene deep-sea benthic Foraminifera and their faunal response to paleoceanographic changes in the eastern Equatorial Pacific
25%121
121-757
121-758
154
154-926
208
208-1262
208-1263
208-1265
208-1267		2012Misra, Sambuddha; Froelich, Philip N.: Lithium isotope history of Cenozoic seawater; changes in silicate weathering and reverse weatheringdownload
25%113
113-689
113-690
114
114-702
119
119-738
119-744
120
120-748
189
189-1172		2012Fioroni, Chiara; Villa, Giuliana et al.: Revised middle Eocene-upper Oligocene calcareous nannofossil biozonation for the Southern Ocean
25%122
122-761
198
198-1209
208
208-1262
208-1263		2012Dinares-Turell, Jaume; Pujalte, Victoriano et al.: The Palaeocene "top chron C27n" transient greenhouse episode; evidence from marine pelagic Atlantic and peri-Tethyan sections
21%175
175-1087		2012Caley, Thibaut; Giraudeau, Jacques et al.: Agulhas leakage as a key process in the modes of Quaternary climate changesdownload
21%198
198-1209
208
208-1265		2012Dedert, Mascha; Stoll, Heather M. et al.: Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)download
18%108
108-659		2012Ufkes, Els; Kroon, Dick: Sensitivity of South-east Atlantic planktonic Foraminifera to mid-Pleistocene climate changedownload
17%16
16-159		2012Wagreich, Michael: "OAE 3"; regional Atlantic organic carbon burial during the Coniacian-Santoniandownload
16%175
175-1078		2012Handiani, Dian; Paul, Andre et al.: Tropical climate and vegetation changes during Heinrich event 1; a model-data comparisondownload
14%171B
171B-1050
210
210-1276		2012Hasegawa, H.; Tada, R. et al.: Drastic shrinking of the Hadley circulation during the Mid-Cretaceous supergreenhousedownload
14%71
71-511
113
113-693		2012Jenkyns, Hugh C.; Schouten-Huibers, L. et al.: Warm Middle Jurassic-Early Cretaceous high-latitude sea-surface temperatures from the Southern Oceandownload
13%175
175-1085		2012Maslin, Mark A.; Pancost, Richard D. et al.: Three and half million year history of moisture availability of South West Africa; evidence from ODP Site 1085 biomarker recordsdownload
11%74
74-525		2012Perez-Rodriguez, Irene; Lees, Jacqueline A. et al.: Planktonic foraminiferal and calcareous nannofossil biostratigraphy and magnetostratigraphy of the uppermost Campanian and Maastrichtian at Zumaia, northern Spaindownload
9%175
175-1078		2012Hessler, Ines; Dupont, Lydie M. et al.: Masked millennial-scale climate variations in south West Africa during the last glaciationdownload
5%3422012Norris, Richard D.; Wilson, Paul A. et al.: Integrated Ocean Drilling Program Expedition 342 preliminary report; Paleogene Newfoundland sediment drifts; 1 June-30 July 2012download
67%2013Richards, P. C.; Stone, P. et al.: Mesozoic magmatism in the Falkland Islands (South Atlantic) and their offshore sedimentary basins
49%177
177-1090
177-1094		2013Jaccard, S. L.; Hayes, C. T. et al.: Two modes of change in Southern Ocean productivity over the past million yearsdownload
43%43
43-384
86
86-577
122
122-761
198
198-1209
208
208-1262		2013Monechi, Simonetta; Reale, Viviana et al.: The Danian/Selandian boundary at Site 1262 (South Atlantic) and in the Tethyan region; biomagnetostratigraphy, evolutionary trends in fasciculiths and environmental effects of the latest Danian event
35%108
108-658
177
177-1094		2013Meckler, A. N.; Sigman, D. M. et al.: Deglacial pulses of deep-ocean silicate into the subtropical North Atlantic Ocean
25%177
177-1090
306
306-U1313		2013Riesselman, Christina R.; Dunbar, Robert B.: Diatom evidence for the onset of Pliocene cooling from AND-1B, McMurdo Sound, Antarctica
20%24
24-237
36
36-328
40
40-362
48
48-400
74
74-525
81
81-553
93
93-605
112
112-688
113
113-690
114
114-702
120
120-748
121
121-752
149
149-897
198
198-1209
199
199-1220		2013Arreguin-Rodriguez, Gabriela J.; Alegret, Laia et al.: Glomospira acme during the Paleocene-Eocene Thermal Maximum; response to CaCO (sub 3) dissolution or to ecological forces?

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