How bioturbation obscured the Cretaceous-Palaeogene boundary record

Author:

Alegret Laia1,Rodríguez-Tovar Francisco J.2,Uchman Alfred3

Affiliation:

1. Departamento Ciencias de la Tierra & IUCA; Universidad de Zaragoza; Campus Plaza San Francisco Zaragoza 50009 Spain

2. Departamento de Estratigrafía y Paleontología; Facultad de Ciencias; Universidad de Granada; Granada 18002 Spain

3. Institute of Geological Sciences; Jagiellonian University; Oleandry Str. 2a Kraków PL-30-063 Poland

Funder

University of Zaragoza

Spanish Ministry of Science and Innovation-FEDER

Junta de Andalucía

Jagiellonian University

Publisher

Wiley

Subject

Geology

Reference36 articles.

1. Recovery of the deep-sea floor after the Cretaceous/Paleogene boundary event: the benthic foraminiferal record in the Basque-Cantabrian basin and in South-eastern Spain;Alegret;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2007

2. Evolución paleoambiental durante el tránsito Cretácico/Paleógeno basada en foraminíferos bentónicos;Alegret;Rev. Español. Paleontol.,2008

3. El corte de Zumaya (España): registro de los foraminíferos bentónicos del Paleógeno inferior;Alegret;Rev. Mex. Cienc. Geol.,2010

4. Cretaceous/Paleogene boundary bathyal paleo-environments in the central North Pacific (DSDP Site 465), the NW Atlantic (ODP Site 1049), the Gulf of Mexico and the Tethys: the benthic foraminiferal record;Alegret;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2005

5. Benthic foraminiferal turnover across the Cretaceous/Paleogene boundary at Agost (southeastern Spain): paleoenvironmental inferences;Alegret;Mar. Micropaleontol.,2003

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