Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Przemysław, Karcz"'
Publikováno v:
Przegląd Geologiczny. 71:224-226
Autor:
Gabriel A. Barberes, Rui Pena dos Reis, Nuno L. Pimentel, André L. D. Spigolon, Paulo E. Fonseca, Przemysław Karcz, Marco C. Azevedo, Maria Teresa Barata
Publikováno v:
Minerals, Vol 11, Iss 8, p 811 (2021)
The Baixo Alentejo Flysch Group (BAFG) is an important stratigraphic unit that covers over half of the South Portuguese Zone (SPZ) depositional area, and it is composed by three main tectono-stratigraphic units: the Mértola, Mira, and Brejeira forma
Externí odkaz:
https://doaj.org/article/f887942ff92647e1854768a81f05d241
Publikováno v:
Geological Quarterly. 66
Autor:
Renata Matlakowska, Przemysław Karcz, Agnieszka Włodarczyk, Aleksandra Sklodowska, Marcin Janas, Robert Stasiuk
Publikováno v:
Environmental Microbiology Reports. 9:459-466
A large part of the organic carbon present in the lithosphere is trapped in fossil organic matter deposited in sedimentary rocks. Only specialized microorganisms are able to degrade it contributing to the return of the carbon to the global cycle. The
Autor:
Robert, Stasiuk, Agnieszka, Włodarczyk, Przemysław, Karcz, Marcin, Janas, Aleksandra, Skłodowska, Renata, Matlakowska
Publikováno v:
Environmental microbiology reports. 9(4)
A large part of the organic carbon present in the lithosphere is trapped in fossil organic matter deposited in sedimentary rocks. Only specialized microorganisms are able to degrade it contributing to the return of the carbon to the global cycle. The
Autor:
Przemysław Karcz
Publikováno v:
Polish Polar Research. 35:41-71
The Passhatten Member (Anisian-Ladinian) is the most westward exposure of the Middle Triassic sedimentary sequence of Spitsbergen. The member has an average organic carbon of 2.21 wt %. The sediments were deposited in a shallow shelf environment unde
Autor:
Przemysław Karcz
Publikováno v:
Polish Polar Research. 31:239-254
Relationships between development of organic-rich shallow shelf facies and variation in isotopic composition of pyrite (Middle Triassic, Spitsbergen) 51 samples from the Middle Triassic black shales (organic carbon-rich silt-stones; up to 4.9% TOC -