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A phylogenetic and morphological study of the genus <i>Dermoloma</i> (<i>Agaricales</i>, <i>Tricholomataceae</i>) in Europe and North America exposes inefficiency of opportunistic species descriptions. [PDF]

IMA Fungus
Adamčíková K, Kiran M, Caboň M, Matheny BP, Sánchez-García M, Arnolds E, Caboňová M, Corriol G, Dima B, Friebes G, Griffith GW, Grootmyers D, Harries D, Karich A, Mešić A, Mihaljevič M, Moreau PA, Pošta A, Shapkin V, Tkalčec Z, Vizzini A, Vondrovicová L, Adamčík S, Jančovičová S.   +23 more
europepmc   +1 more source

Rimski akvedukti na otoku Pagu [PDF]

, 2008
Boris Ilakovac
core   +1 more source

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“Unusual relief forms“ on Velebit Mt., Croatia

2010
Located along the Adriatic coast, the Velebit Mt. is the largest mountain range in Croatia. As a part of extensive Dinaric karst region, it consists of a wide variety of stratigraphic units, ranging in age from Carboniferous to Quaternary. Structurally, Velebit Mt. represents an anticline built up predominantly of carbonate rocks.
Dražen, Perica, Krklec, Kristina, Lozić, Sanja   +2 more
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Fluviokarst of Velebit Mt. (Croatia)

2001
The origin and evolution of fluviokarst features on Velebit Mt. is conditioned by hydrogeological beds that build it. Since most of its structure is developed in permeable limestone beds fluviokarst forms are rare. Besides hydrogeological characteristics of the beds important role in their development has slope inclination.
Buzjak, Nenad, Perica, Dražen
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Cave register of North Velebit mt.

2011
jeverni Velebit izrazito je krško područje, a površina terena u potpunosti je izgrađena od okršavanju podložnih karbonatnih stijena: mezozojskih vapnenaca i dolomita, te tercijarnih karbonatnih breča (Velić & Velić, 2009). Krški masiv Sjevernog Velebita omeđen je ponornim područjima rijeka Like i Gacke s istočne te obalom mora sa zapadne strane.
Stroj, Andrej, Bakšić, Darko, Paar, Dalibor   +2 more
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Bizarre karst landforms on Velebit Mt.

2005
Carbonate substrate of the Velebit Mt. karst favoured development of some bizarre landforms. The carbonate rocks exposed on the Velebit Mt. date from Middle Permian age (but exposed only in a small area) to Eocene-Oligocene age. The outcrops reveal varieties of limestones, calcareous dolomites, dolomites and carbonate breccias. The odd-shaped (bizarre)
Marjanac, Tihomir, Perica, Dražen, Husnjak, Stjepan   +2 more
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Middle Permian calcispongal cement reef on the Velebit Mt

Vijesti Hrvatskoga geološkog društva, 2000
Middle Permian “middle zone of black limestones” exposed near Baške Oštarije on the Velebit Mt. is reinterpreted as ecological and morphological calcispongite reef. The reef framework is made of fenestellid bryozoans and calcisponges. It is possible to recognize two overgrowth generations.
Sremac, Jasenka, Marjanac, Tihomir
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Geochemical evidence for environmental changes at the Permian–Triassic transition, Mt. Velebit, Croatia

Geochimica et Cosmochimica Acta, 2006
A detailed geochemical study, based on carbonate and associated organic carbon isotope composition, major and trace elements (including REE) distribution, the abundance and carbon isotope composition of hydrocarbon biomarkers, provides insights into the environmental changes at the Permian− Triassic (P/Tr) transition in the Velebit Mt., Croatia ...
Fio, Karmen, Spangenberg, Jorge E., Sremac, Jasenka, Vlahović, Igor, Velić, Ivo, Mrinjek, Ervin   +5 more
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Geology of the Central Velebit Mt.(Croatia)

Lička revija, 2005
Velebit se u geološkom smislu, kao dio krških Dinarida i Jadranske karbonatne platforme, sastoji od sedimenata vrlo velikog raspona starosti: od karbona (oko 320 milijuna godina) pa do oligocena (oko 24 milujuna godina), ukupne debljine od gotovo 10.000 m.
openaire