about
sameAs
The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundaryEvidence for global cooling in the Late Cretaceous.Blooms of aberrant planktic foraminifera across the K/Pg boundary in the Western Tethys: causes and evolutionary implicationsNew species of the genus Trochoguembelitria from the lowermost Danian of Tunisia – biostratigraphic and evolutionary implications in planktonic foraminiferaEnvironmental distribution of post-Palaeozoic crinoids from the Iberian and south-Pyrenean basins (NE Spain)Multi-proxy record of the Chicxulub impact at the Cretaceous-Paleogene boundary from Gorgonilla Island, ColombiaCretaceous-Paleogene boundary deposits at Loma Capiro, central Cuba: Evidence for the Chicxulub impactResponse--Cretaceous ExtinctionsChronostratigraphy and new vertebrate sites from the upper Maastrichtian of Huesca (Spain), and their relation with the K/Pg boundaryDid Late Cretaceous cooling trigger the Campanian–Maastrichtian Boundary Event?Revalidation of the genus Chiloguembelitria Hofker: Implications for the evolution of early Danian planktonic foraminiferaBenthic origin and earliest evolution of the first planktonic foraminifera after the Cretaceous/Palaeogene boundary mass extinctionMaastrichtian−basal Paleocene charophyte biozonation and its calibration to the Global Polarity Time Scale in the southern Pyrenees (Catalonia, Spain)Tidal influence in redbeds: A palaeoenvironmental and biochronostratigraphic reconstruction of the Lower Tremp Formation (South-Central Pyrenees, Spain) around the Cretaceous/Paleogene boundaryDinoflagellate biostratigraphy at the Campanian-Maastrichtian boundary in Zumaia, northern SpainPlanktonic foraminiferal and calcareous nannofossil biostratigraphy and magnetostratigraphy of the uppermost Campanian and Maastrichtian at Zumaia, northern SpainSmooth and rugose wall textures in earliest Danian trochospiral planktic foraminifera from TunisiaCatastrophic mass extinction and assemblage evolution in planktic foraminifera across the Cretaceous/Paleogene (K/Pg) boundary at Bidart (SW France)Chicxulub impact event is Cretaceous/Paleogene boundary in age: New micropaleontological evidenceA new high‐resolution planktic foraminiferal zonation and subzonation for the lower DanianCretaceous-Tertiary boundary planktic foraminiferal mass extinction and biochronology at La Ceiba and Bochil, Mexico, and El Kef, TunisiaQuantifying the evolutionary turnover across the K-T boundary catastrophic planktic foraminiferal extinction event at El Kef, TunisiaThe Cretaceous/Tertiary boundary: sedimentology and micropalaeontology at El Mulato section, NE MexicoChapter C5b Planktic foraminiferal quantitative analysis across the Campanian/Maastrichtian boundary at Tercis (Landes, France)Chapter C5d Campanian-Maastrichtian planktonic foraminifera at Tercis les Bains (Landes, France); synthetic view and potential for global correlationMicropaleontology and sedimentology across the Cretaceous/Tertiary boundary at La Ceiba (Mexico): impact-generated sediment gravity flowsSpanish and Tunisian Cretaceous/Tertiary boundary sections: A planktic foraminiferal biostratigraphic comparison and evolutionary eventsThe Cretaceous/Tertiary boundary mass extinction in planktic foraminifera at Agost, (Spain)
P50
Q28274950-7020EE45-559F-4887-AC9D-2E19B1FC364BQ42230663-EC79A680-5538-4118-8BDB-F8B0C761DACAQ56520754-52CA0509-9FC2-4385-BDBB-03DC7B9F0E94Q56521896-EA3F9E19-6009-4EDA-BC0A-4CEB82971466Q57258344-5977baee-4e8e-5bd4-9d9c-8e87bb00d367Q57967645-D2317654-BFFB-45CD-A324-307F1BCBB64CQ58457572-6F65018C-E202-486C-8328-B4BACC0E60B4Q59791433-B97C99EC-78C6-4453-98F0-6F16442737AEQ59995656-E5995B26-BAA0-4367-9EA4-E2F751562ADCQ59995660-2D58ED56-5D3A-42CA-A2AA-CB895091E7DDQ59995666-C978B698-A24C-4E55-AA72-D27345D26029Q59995669-27E4D3D6-99B0-4C0A-BB25-A87EBDDB1E16Q59995677-FEA21A46-A7E9-4D51-B7E1-034AED22670EQ59995681-63735301-5C1A-424C-AE94-1C4E861042F1Q59995685-74F16897-67FB-47EF-8A22-8BCDAE8E9E42Q59995692-0E313F40-C0D7-4206-9720-EC004FB5F35EQ59995695-4ADB7C6C-2011-4074-AE7D-9393CFE0001EQ59995699-63940063-A807-40A5-856F-5116932CD864Q59995703-70030F95-5058-49D0-8CBF-CA6158CB665CQ59995708-053D2BF2-AF4A-4B20-AEA4-2DCC3FB13BD8Q59995718-AEE2F60F-4D13-4FAE-AEBE-A1E9A500EC2AQ59995723-D5DCACFD-7C3A-4F1F-8EF5-1783F927FBD3Q59995727-09549484-054B-44FA-A724-3D04EF0DF593Q59995732-C32495B4-A32A-4235-9B61-AA2EB7FDA49EQ59995735-06146274-6B71-4367-B5D3-EE5B63EA714EQ59995741-2b148002-451a-beb1-634d-78bdd2e8a900Q59995746-1AFF7211-E29C-4F1B-BF7A-210004E573C2Q59995757-3450ECBF-8E2A-4501-911F-BEC8924FAF8E
P50
description
hulumtues
@sq
researcher
@en
ricercatore
@it
wetenschapper
@nl
հետազոտող
@hy
name
José A. Arz
@ast
José A. Arz
@en
José A. Arz
@es
José A. Arz
@nl
José A. Arz
@sl
type
label
José A. Arz
@ast
José A. Arz
@en
José A. Arz
@es
José A. Arz
@nl
José A. Arz
@sl
altLabel
J. A. Arz
@en
J.A. Arz
@en
José Arz
@en
prefLabel
José A. Arz
@ast
José A. Arz
@en
José A. Arz
@es
José A. Arz
@nl
José A. Arz
@sl
P106
P1153
6602096392
P2038
P21
P214
18156616966828590818
P31
P496
0000-0003-0063-8752