about
Environmental Predictors of Diversity in Recent Planktonic Foraminifera as Recorded in Marine SedimentsThe impact of Cenozoic cooling on assemblage diversity in planktonic foraminiferaA Palaeogene perspective on climate sensitivity and methane hydrate instability.Gas hydrates: past and future geohazard?A Cenozoic record of the equatorial Pacific carbonate compensation depth.Comment on "Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a".Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal MaximumCO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilizationExtinction and environmental change across the Eocene-Oligocene boundary in TanzaniaDynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal MaximumOrbital forcing of terrestrial hydrology, weathering and carbon sequestration during the Palaeocene-Eocene Thermal MaximumAssessing the Past and Future Stability of Global Gas Hydrate ReservoirsExceptionally well preserved upper Eocene to lower Oligocene calcareous nannofossils (Prymnesiophyceae) from the Pande Formation (Kilwa Group), TanzaniaMajor shifts in calcareous phytoplankton assemblages through the Eocene-Oligocene transition of Tanzania and their implications for low-latitude primary productionStratigraphy and sedimentology of the Upper Cretaceous to Paleogene Kilwa Group, southern coastal TanzaniaReply to comment on “Magnitude and profile of organic carbon isotope records from the Paleocene–Eocene Thermal Maximum: Evidence from northern Spain” by Manners et al. [Earth Planet. Sci. Lett. 376 (2013) 220–230]Magnitude and profile of organic carbon isotope records from the Paleocene–Eocene Thermal Maximum: Evidence from northern SpainMethane Hydrate Instability: A View from the PalaeogeneTrace metal (Mg/Ca and Sr/Ca) analyses of single coccoliths by Secondary Ion Mass SpectrometryTemporal buffering of climate-driven sediment flux cycles by transient catchment responseComment on “What do we know about the evolution of Mg to Ca ratios in seawater?” by Wally Broecker and Jimin YuThe micropalaeontological record of global changePost-sampling dissolution and the consistency of nannofossil diversity measures: A case study from freshly cored sediments of coastal TanzaniaCalcareous nannofossil assemblages of the Late Cretaceous Fiqa Formation, north OmanLarge Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change
P50
Q28595623-D665173A-8BED-4059-A5E0-20323124074BQ28601780-1B83593D-573A-4FD8-878B-AE7625773AEBQ37733940-6074EB83-2151-411C-8201-5CDBE6EB67D5Q39881627-32865346-8D37-4021-A0F0-423865244E61Q41973994-504A3F1F-6C4F-4FDD-98DE-2F84C7AA080DQ46294162-725B609E-E4B5-4246-9632-A420817BB9DAQ53100238-55EBB6D6-5E0D-4020-98B6-CFDF2C130367Q53100360-3BF6B7C0-D161-4150-8C6C-9C2F4FAB06D5Q53997701-C1540F92-694A-40E7-97B4-2B94A551DF6EQ57857591-BDB3BFD3-15BC-4E38-98BD-10ED721EE53EQ57857625-7EA30B94-6BE2-4101-A84C-6B0EEF324E9BQ57915227-469E4261-B94B-44CC-A1C1-C1924B17F8D8Q58053995-A8882595-4B7E-4A53-B828-0A7B1D8DCB3AQ58054009-DAB42377-2349-4A04-A4E1-641A12ABB472Q58054030-ECD8C555-27AC-46E8-8F9F-CEBB6188425FQ58097875-A1AD676E-00A2-4AD4-8BA1-DDC071487C9CQ58097937-5D9796F2-ED8A-4D2F-9E75-92868057DA77Q58422103-B96EEFA0-43D4-4930-B621-D247644904C6Q59308764-0966DAFA-4967-42BD-98D8-B02C565C341AQ59308770-AB242522-79E7-4B87-A084-DDA12E417CEAQ59308778-678F7B77-024F-4EF5-B51A-FAF21FC2FE41Q59308781-E53A34BF-053A-472A-AF32-DEDF53BF0569Q59308793-640132BA-B1D3-44F3-8C89-578BB00B548CQ63071710-49B9C457-0397-46C3-A645-5C6B0D92086FQ91717130-BF3616FB-988B-46FC-8CC2-8FD98270EE53
P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Tom Dunkley Jones
@ast
Tom Dunkley Jones
@en
Tom Dunkley Jones
@es
Tom Dunkley Jones
@nl
Tom Dunkley Jones
@sl
type
label
Tom Dunkley Jones
@ast
Tom Dunkley Jones
@en
Tom Dunkley Jones
@es
Tom Dunkley Jones
@nl
Tom Dunkley Jones
@sl
prefLabel
Tom Dunkley Jones
@ast
Tom Dunkley Jones
@en
Tom Dunkley Jones
@es
Tom Dunkley Jones
@nl
Tom Dunkley Jones
@sl
P106
P1153
55660519500
P31
P496
0000-0002-9518-8143