Kullberg, J. C., Rocha R. B., Soares A. F., Rey J., Terrinha P., Azerêdo A. C., Callapez P., Duarte, L.V., Kullberg M. C., Martins L., Miranda J. R., Alves C., Mata J., Madeira J., Mateus O., Moreira M., & Nogueira C. R.
(2013).
A Bacia Lusitaniana: Estratigrafia, Paleogeografia e Tectónica.
(
Dias, R. Araújo, A, Terrinha, P. and Kullberg, J. C., Ed.).
Geologia de Portugal no contexto da Ibéria. Volume II. 195-350., Lisboa: Escolar Editora
da} Rocha, {R. E. B., Kullberg {J. C. R. }, & Mateus O.
(2013).
A Bacia Lusitaniana: Estratigrafia, Paleogeografia e Tectónica.
(
Dias, Araújo, R., A, Terrinha, P., Kullberg, {J. C.}, Ed.).
Geologia de Portugal no contexto da Ibéria. 195–347., 1: Escolar Editora
Abstractn/a
Mateus, O., Callapez P. M., Polcyn M. J., Schulp A. S., Gonçalves A. O., & Jacobs L. L.
(2019).
The Fossil Record of Biodiversity in Angola Through Time: A Paleontological Perspective.
(
Huntley, Brian J., Russo, Vladimir, Lages, Fernanda, Ferrand, Nuno, Ed.).
Biodiversity of Angola: Science & Conservation: A Modern Synthesis. 53–76.: Springer International Publishing
AbstractThis chapter provides an overview of the alpha paleobiodiversity of Angola based on the available fossil record that is limited to the sedimentary rocks, ranging in age from Precambrian to the present. The geological period with the highest paleobiodiversity in the Angolan fossil record is the Cretaceous, with more than 80{%} of the total known fossil taxa, especially marine molluscs, including ammonites as a majority among them. The vertebrates represent about 15{%} of the known fauna and about one tenth of them are species firstly described based on specimens from Angola.
Mateus, O., Callapez P. M., Polcyn M. J., Schulp A. S., Gonçalves A. O., & Jacobs L. L.
(2019).
The Fossil Record of Biodiversity in Angola Through Time: A Paleontological Perspective.
(
Huntley, Brian J., Russo, Vladimir, Lages, Fernanda, Ferrand, Nuno, Ed.).
Biodiversity of Angola: Science {&} Conservation: A Modern Synthesis. 53–76., Cham: Springer International Publishing
AbstractThis chapter provides an overview of the alpha paleobiodiversity of Angola based on the available fossil record that is limited to the sedimentary rocks, ranging in age from Precambrian to the present. The geological period with the highest paleobiodiversity in the Angolan fossil record is the Cretaceous, with more than 80{%} of the total known fossil taxa, especially marine molluscs, including ammonites as a majority among them. The vertebrates represent about 15{%} of the known fauna and about one tenth of them are species firstly described based on specimens from Angola.
Salminen, J., Dinis J., & Mateus O.
(2014).
Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal.
(
Rogério Rocha, João Pais, José Carlos Kullberg, Stanley Finney, Ed.).
STRATI 2013 First International Congress on Stratigraphy At the Cutting Edge of Stratigraphy. 873-877., Heidelberg New York Dordrecht London: Springer
AbstractWe present a stratigraphic log supporting a preliminary magnetostratigraphy of a Tithonian–Berriasian section in Porto da Calada (Portugal). Based on biostratigraphy and reversed and normal magnetostratigraphy, the location of the Tithonian–Berriasian boundary is tentatively located at ca. 52 m, not in disagreement
with former proposals. Due to the occurrence of later remagnetization (diagenesis), the magnetostratigraphic definition of the Tithonian–Berriasian section at the Cabo Espichel (Portugal) location was not able to be established.
] 
