Facies heterogeneity of a Kimmeridgian Carbonate Ramp (Jabaloyas, eastern Spain): a combined outcrop and 3D geomodelling analysis.

Contribution of drone photogrammetry to 3D outcrop modeling of facies, porosity, and permeability heterogeneities in carbonate reservoirs (Paris Basin, Middle Jurassic)

“…Ehrenberg et al, 2006aEhrenberg et al, , 2006bRankey et al, 2006;Harris, 2010;Palermo et al, 2010;Amour et al, 2012;Gasparrini et al, 2017;Tomassetti et al, 2018). Amour et al, (2012Amour et al, ( , 2013 in 3D to better understand the meter-scale facies architecture of the deposits and their heterogeneity (Lipinski et al, 2013;Benson et al, 2014;San Miguel et al, 2014;Tomassetti et al, 2018;Brandano et al, 2020). The development of drone photogrammetry in recent years has eased the quantitative analysis of geological outcrops, even along cliff faces (Schmitz et al, 2014;Cabello et al, 2018;Rubi et al, 2018;Nesbit et al, 2018;Siddiqui et al, 2019).…”

Development of coral–sponge–microbialite reefs in a coated grain-dominated carbonate ramp (Upper Jurassic, eastern Sardinia, Italy)

“…The widespread presence of debris deriving from the bioconstructions in facies F8 and F9 testifies that they were periodically exposed to storms and currents. San Miguel et al (2013) interpreted deposits similar to F8 in the Kimmeridgian of the Iberian Basin as derived from storm-induced flows probably below the fair-weather wave base. Debris sheets rich in reefal material were frequently deposited following storm erosion and disintegration of the reefs (Bertling and Insalaco 1998).…”

Reply to Comment by John J.G. Reijmer on ‘Understanding carbonate factories through palaeoecological and sedimentological signals – Tribute to Luis Pomar’ by Brandano et al. (2022), Sedimentology, 69, 5–23

“…), LBF and diverse heterozoan biota (Mateu‐Vicens et al ., 2012; Morsilli et al ., 2012; Pomar et al ., 2014; Shabafrooz et al ., 2014). During the Cretaceous, corals thrived with rudist bivalves (Skelton et al ., 1997; Johnson & Kauffman, 2001; Pomar et al ., 2005), and during the Jurassic with microbes and stromatoporoids (Leinfelder et al ., 2002; San Miguel et al ., 2013; Nembrini et al ., 2020). Thus, the use of obligatory autotrophic components such as red and green algae is the best approach for the definition of light‐based bathymetric zones, and this seems to be valid for the Cenozoic, most of the Mesozoic and even the late Palaeozoic (e.g.…”