Prasinophyte bloom and putative fungi abundance near the Kačák event (Middle Devonian) from the Odivelas Limestone, Southwest Iberia

0532511 - GLÚ 2021 RIV DE eng J - Článek v odborném periodiku
Machado, G. - Slavík, Ladislav - Moreira, N. - Fonseca, P. E.
Prasinophyte bloom and putative fungi abundance near the Kačák event (Middle Devonian) from the Odivelas Limestone, Southwest Iberia.
Palaeobiodiversity and Palaeoenvironments. Roč. 100, č. 3 (2020), s. 593-603. ISSN 1867-1594. E-ISSN 1867-1608
Institucionální podpora: RVO:67985831
Klíčová slova: Ossa-Morena Zone * Eifelian-Givetian * Palynology * Conodonts * Biotic crisis
Obor OECD: Paleontology
Impakt faktor: 1.406, rok: 2020
Způsob publikování: Open access
https://link.springer.com/article/10.1007%2Fs12549-019-00415-1

The Kačák Event is one of the several prominent Devonian climatic and biotic perturbations with a supra-regional to global extent. Its record can be traced in the litho- and biostratigraphy of uppermost Eifelian-lowermost Givetian strata and with multiple geochemical and geophysical proxies. In southwest Iberia, within southwestern Ossa-Morena Zone domains, there are rare, scattered Early-Middle Devonian limestone occurrences. One of these occurrences—the Odivelas Limestone type locality—is revisited in terms of conodont biostratigraphy and palynology and the results compared with previous data on reef macrofauna and magnetic susceptibility stratigraphy. The new data show that this locality is probably within the Polygnathus hemiansatus zone, i.e. of the earliest Givetian age. The palynological content of a ca. 2 m of black, organic-rich, fine grained limestone section is dominated, in varied proportions, by amorphous organic matter, putative fungal hyphae, and prasinophycean algae. The results are interpreted as an indication of high organic productivity and deposition in hypoxic to anoxic settings and probable biotic crisis, in both marine and terrestrial realms, connected with the Middle Devonian Kačák Event. The similarity of this record with other Devonian events is discussed.
Trvalý link: http://hdl.handle.net/11104/0310981