FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3174755429> ?p ?o ?g. }

• W3174755429 endingPage "203" @default.
• W3174755429 startingPage "163" @default.
• W3174755429 abstract "This contribution provides a comparison between laminated microbial structures formed in saline lacustrine environments (lower and middle Miocene in the Sierra de Alcubierre and Montes de Castejón) and fluvial to fluvio-lacustrine environments (middle to upper Miocene in the Muela de Borja and Montolar hill), in the Ebro Basin. Saline and freshwater conditions were deduced from sedimentological features and stable isotope composition (δ13C and δ18O) of the carbonate facies. Primarily the focus is on laminae and lamination: shape, thickness, textural features, and lamina arrangement.In the saline carbonate lacustrine record, stromatolites and rare oncolites consist of calcite and dolomite, and occur as thin planar, domed, and stratiform stromatolites. These forms are always associated with laminated limestones and dolostones that include ripple and horizontal lamination, and hummocky cross-stratification. In the microbialites, micrite, microsparite, and sparite define three types of simple laminae that generally are grouped into composite dark and light laminae. The laminae are thin, flat to slightly undulate, with very smooth cross-sectional shapes. Preserved microbial components are rare and, when present, consist of loose filamentous bodies or rare tubes sub-perpendicular to lamination.In the freshwater environment (open-lake and fluvial record) abundant oncolites, calcite-coated stems and minor stromatolites consist of low-Mg calcite. These components formed in gently channeled streams and open lakes, with tufaceous palustrine fringes. The shape of oncolites reflects the morphology of the nuclei. The laminae consist of micrite, microsparite, and sparite, forming simple and composite laminae. The laminae are generally thick, gently undulate to wavy in cross section. There are multiple ranges of lamination. Microbial bush-shaped and fan-shaped bodies, set perpendicular to sub-perpendicular to lamination, are abundant, which makes the laminae wavy to crinkly and porous.It is suggested that salinity exerted some control on the types of microbes and/or their style of development, which impacted the geometry of the laminae. In all cases, the lamina arrangement into cycles can record seasonal to multi-annual changes in climate parameters. In contrast, gross morphology of microbialites was highly influenced by depth and hydrodynamics, and largely by the nucleus morphology in the case of oncolites and stem coatings." @default.
• W3174755429 created "2021-07-05" @default.
• W3174755429 creator A5010126856 @default.
• W3174755429 creator A5026157949 @default.
• W3174755429 creator A5032667444 @default.
• W3174755429 creator A5054242786 @default.
• W3174755429 creator A5075336155 @default.
• W3174755429 date "2021-01-01" @default.
• W3174755429 modified "2023-10-01" @default.
• W3174755429 title "Lacustrine and Fluvial Carbonate Microbialites in the Neogene of the Ebro Basin, Spain: A Summary of Up-to-Date Knowledge" @default.
• W3174755429 cites W123675920 @default.
• W3174755429 cites W145520293 @default.
• W3174755429 cites W1512318619 @default.
• W3174755429 cites W1635581289 @default.
• W3174755429 cites W17774365 @default.
• W3174755429 cites W1931629071 @default.
• W3174755429 cites W1935511639 @default.
• W3174755429 cites W1967764929 @default.
• W3174755429 cites W1969563020 @default.
• W3174755429 cites W1970200726 @default.
• W3174755429 cites W1977545230 @default.
• W3174755429 cites W1977934443 @default.
• W3174755429 cites W1979800212 @default.
• W3174755429 cites W1981161040 @default.
• W3174755429 cites W1981232537 @default.
• W3174755429 cites W1993941581 @default.
• W3174755429 cites W1997588493 @default.
• W3174755429 cites W2011798276 @default.
• W3174755429 cites W2012776694 @default.
• W3174755429 cites W2016562298 @default.
• W3174755429 cites W2016741303 @default.
• W3174755429 cites W2023346087 @default.
• W3174755429 cites W2028709543 @default.
• W3174755429 cites W2030070538 @default.
• W3174755429 cites W2030955225 @default.
• W3174755429 cites W2036384349 @default.
• W3174755429 cites W2048631674 @default.
• W3174755429 cites W2052484256 @default.
• W3174755429 cites W2052841019 @default.
• W3174755429 cites W2056880513 @default.
• W3174755429 cites W2058328029 @default.
• W3174755429 cites W2062740614 @default.
• W3174755429 cites W2064200453 @default.
• W3174755429 cites W2067407405 @default.
• W3174755429 cites W2068486477 @default.
• W3174755429 cites W2071869120 @default.
• W3174755429 cites W2084560015 @default.
• W3174755429 cites W2085103921 @default.
• W3174755429 cites W2085246620 @default.
• W3174755429 cites W2087361151 @default.
• W3174755429 cites W2087900760 @default.
• W3174755429 cites W2088897561 @default.
• W3174755429 cites W2092867256 @default.
• W3174755429 cites W2094057540 @default.
• W3174755429 cites W2096522903 @default.
• W3174755429 cites W2127356739 @default.
• W3174755429 cites W2130892566 @default.
• W3174755429 cites W2140338234 @default.
• W3174755429 cites W2149736100 @default.
• W3174755429 cites W2150772200 @default.
• W3174755429 cites W2171229333 @default.
• W3174755429 cites W2171479207 @default.
• W3174755429 cites W2197816285 @default.
• W3174755429 cites W2294030845 @default.
• W3174755429 cites W2295565092 @default.
• W3174755429 cites W2312604399 @default.
• W3174755429 cites W2318042047 @default.
• W3174755429 cites W2332701509 @default.
• W3174755429 cites W2345679332 @default.
• W3174755429 cites W2346794258 @default.
• W3174755429 cites W2522006303 @default.
• W3174755429 cites W2523581566 @default.
• W3174755429 cites W2538373424 @default.
• W3174755429 cites W2595392311 @default.
• W3174755429 cites W2788262167 @default.
• W3174755429 cites W2800547640 @default.
• W3174755429 cites W2804961812 @default.
• W3174755429 cites W2909579427 @default.
• W3174755429 cites W2950531536 @default.
• W3174755429 cites W32039489 @default.
• W3174755429 cites W4211046001 @default.
• W3174755429 cites W4240105918 @default.
• W3174755429 cites W968584127 @default.
• W3174755429 doi "https://doi.org/10.1007/978-3-030-66576-0_6" @default.
• W3174755429 hasPublicationYear "2021" @default.
• W3174755429 type Work @default.
• W3174755429 sameAs 3174755429 @default.
• W3174755429 citedByCount "0" @default.
• W3174755429 crossrefType "book-chapter" @default.
• W3174755429 hasAuthorship W3174755429A5010126856 @default.
• W3174755429 hasAuthorship W3174755429A5026157949 @default.
• W3174755429 hasAuthorship W3174755429A5032667444 @default.
• W3174755429 hasAuthorship W3174755429A5054242786 @default.
• W3174755429 hasAuthorship W3174755429A5075336155 @default.
• W3174755429 hasConcept C109007969 @default.
• W3174755429 hasConcept C112959462 @default.
• W3174755429 hasConcept C127313418 @default.
• W3174755429 hasConcept C146588470 @default.

• next