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409 Publications found! (Query time: 0.003 s)Download as CSV fileDownload as KML file

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ScoreExp/Site/HoleYear Author/TitleFull text
28%41
41-366
113
113-689
2012Rabideaux, Nathan; Cramer, Benjamin S. et al.: Opening of circum-Antarctic gateways and the evolution of deepwater circulation at eastern Equatorial Atlantic DSDP Site 366 (40-33 Ma)
28%113
113-690
2012Storme, Jean-Yves; Devleeschouwer, Xavier et al.: The Palaeocene/Eocene boundary section at Zumaia (Basque-Cantabric Basin) revisited; new insights from high-resolution magnetic susceptibility and carbon isotope chemostratigraphy on organic matter (delta (super 13) C (sub org) )
23%113
113-689
115
115-711
119
119-738
2012Chang, Liao; Roberts, Andrew P. et al.: Giant magnetofossils and hyperthermal events
23%113
113-689
145
145-884
207
207-1260
2012Borrelli, Chiara; Cramer, Benjamin S. et al.: Ocean circulation in the northwestern Pacific (ODP Site 884) from the middle Eocene to the early Oligocene (45-33 Ma)
23%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
6%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
23%113
113-689
113-690
113-693
119
119-737
119-738
119-744
119-745
119-746
120
120-747
120-748
120-751
183
183-1138
2013Renaudie, Johan; Lazarus, David B.: New species of Neogene radiolarians from the Southern Ocean; Part II
23%113
113-689
113-690
113-693
119
119-744
120
120-747
120-748
120-751
183
183-1138
2013Renaudie, Johan; Lazarus, David B.: On the accuracy of paleodiversity reconstructions; a case study in Antarctic Neogene radiolarians
19%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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