Agata Jurkowska

发表

The relation of a coastal environment to early diagenetic clinoptilolite (zeolite) formation - New data from the Late Cretaceous European Basin

M. Barski, E. Worobiec, Agata Jurkowska, 2019, Palaeogeography, Palaeoclimatology, Palaeoecology.

Inoceramid stratigraphy and depositional architecture of the Campanian and Maastrichtian of the Miechów Synclinorium (southern Poland)

Agata Jurkowska, 2016 .

Taphonomic differentiation of Oxfordian ammonites from the Cracow Upland, Poland

B. Kołodziej, Agata Jurkowska, 2013, Paläontologische Zeitschrift.

The trace fossil Lepidenteron lewesiensis: a taphonomic window on diversity of Late Cretaceous fishes

A. Uchman, Agata Jurkowska, M. Bieńkowska-Wasiluk, 2015, Paläontologische Zeitschrift.

The role of biogenic silica in the formation of Upper Cretaceous pelagic carbonates and its palaeoecological implications

M. Bąk, Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2019, Cretaceous Research.

A RECORD OF SEQUESTRATION OF PLANT MATERIAL BY MARINE BURROWING ANIMALS AS A NEW FEEDING STRATEGY UNDER OLIGOTROPHIC CONDITIONS EVIDENCED BY PYRITE MICROTEXTURES

A. Uchman, Agata Jurkowska, Ewa ŚWIERCZEWSKA-GŁADYSZ, 2018, Palaios.

New model of Si balance in the Late Cretaceous epicontinental European Basin

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2020 .

The trace fossil Lepidenteron lewesiensis (Mantell, 1822) from the Upper Cretaceous of southern Poland

A. Uchman, Agata Jurkowska, 2013 .

Occurrence and paleoecological significance of lyssacinosid sponges in the Upper Cretaceous deposits of southern Poland

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2013, Facies.

Maastrichtian island in the central European Basin—new data inferred from palynofacies analysis and inoceramid stratigraphy

M. Barski, Agata Jurkowska, 2017, Facies.

Carbon isotopes, palynology and stratigraphy of the Santonian – Campanian boundary: the GSSP auxiliary sections, Seaford Head (England) and Bocieniec (Poland), and correlation between the Boreal and Tethyan realms

I. Jarvis, C. Ullmann, N. Thibault, 2022, Cretaceous Research.

Opoka – a mysterious carbonate-siliceous rock: an overview of general concepts

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2022, Geology, Geophysics and Environment.

The Biotic‐Abiotic Control of Si Burial in Marine Carbonate Systems of the Pre‐Eocene Si Cycle

Agata Jurkowska, 2022, Global Biogeochemical Cycles.

Porosphaera globularis (Phillips, 1829) (Porifera, Calcarea) in the Campanian (Upper Cretaceous) of extra-Carpathian Poland

Agata Jurkowska, Danuta Olszewska-Nejbert, Zofia Dubicka, 2015 .

An integrated stratigraphic study across the Santonian/Campanian boundary at Bocieniec, southern Poland: A new boundary stratotype candidate

P. Gorzelak, Krystian Wójcik, N. Thibault, 2017 .

Improving detection of foraminifera by cathodoluminescence

B. Kołodziej, M. Banaś, Agata Jurkowska, 2011 .

Evolution of Late Cretaceous Si cycling reflected in the formation of siliceous nodules (flints and cherts)

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2020 .

Campanian (Late Cretaceous) Theonellidae and Phymaraphiniidae (lithistid Demospongiae) from the Miechów and Mogilno‐Łódź synclinoria (southern and central Poland): new data and taxonomic revision

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2022, Papers in Palaeontology.

Life beneath ammonite shells – A unique Late Cretaceous habitat for the trace maker of Chondrites and its impact on taphonomy of the shells

A. Uchman, M. Banaś, Agata Jurkowska, 2017 .

New data about the Turonian–Coniacian sponge assemblage from Central Europe

R. Niedźwiedzki, Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2019, Cretaceous Research.

Plant assemblage from Opole, southern Poland: New data on Late Cretaceous vegetation of the northern part of the European Province

P. Gedl, E. Worobiec, B. Płachno, 2018 .

Antitrust Private Enforcement – Case of Poland

Agata Jurkowska, 2008 .

The evolution of the marine Si cycle in the Archean-Palaeozoic - an overlooked Si source?

Agata Jurkowska, Ewa Świerczewska‐Gładysz, 2023, Earth-Science Reviews.