Results 161 to 170 of about 4,290 (216)

Frasnian carbonate mounds of the Frasnes area, Belgium

, 2004
openaire   +2 more sources

High extinction risk in large foraminifera during past and future mass extinctions. [PDF]

Sci Adv
Feng Y, Song H, Song H, Wu Y, Li X, Tian L, Dong S, Lei Y, Clapham ME.   +8 more
europepmc   +1 more source

A deep dive into the coelacanth phylogeny. [PDF]

PLoS One
Ferrante C, Cavin L.
europepmc   +1 more source

Frasnian coral- stromatoporoid-microbial atolls, Belgium

, 2007
openaire   +1 more source

Any catastrophic Event at the Frasnian-Famennian Boundary ?

, 1997
Thomalla, E., Streel, Maurice, Vanguestaine, Michel   +2 more
openaire   +1 more source

Tempo of the Late Ordovician mass extinction controlled by the rate of climate change. [PDF]

Sci Adv
Zhang Z, Yang C, Sahy D, Zhan RB, Wu RC, Li Y, Deng Y, Huang B, Condon DJ, Rong J, Li XH.   +10 more
europepmc   +1 more source

Organic Sulfur Markers as Proxies of Depositional Paleoeenvironments Related to Recôncavo and Amazon Basins, Brazil. [PDF]

ACS Omega
Nery do Amaral D, Miranda FLEC, de Oliveira LML, Cerqueira JR, Ribeiro HJPS, Oliveira OMC, Queiroz AFS, Ferreira SLC, Machado ME.   +8 more
europepmc   +1 more source

Tsunamis triggered the Late Frasnian Kellwasser extinction event

, 2014
Poty, Edouard, Denayer, Julien, Mottequin, Bernard   +2 more
openaire   +1 more source

Late Frasnian stromatactis-coral-microbial carbonate mounds, Belgium

, 2007
openaire   +1 more source

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Carbon isotope geochemistry of the Frasnian–Famennian transition

Palaeogeography, Palaeoclimatology, Palaeoecology, 2002
Abstract Carbon isotope records for inorganic and total organic carbon (TOC) as well as for individual organic biomarkers show two positive excursions in the Late Frasnian with comparable shape and amplitude in δ13C. The positive shifts in δ13C can be correlated with the deposition of the Kellwasser horizons.
Rich Pancost
exaly   +3 more sources