FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3044281872> ?p ?o ?g. }

• W3044281872 endingPage "173" @default.
• W3044281872 startingPage "129" @default.
• W3044281872 abstract "1.The microgranular/agglutinated imperforate larger foraminifera (ILF, chiefly “lituolids”) of Mesozoic shallow marine carbonate shelves are a polyphyletic group of K-strategists, ecologically homogeneous inhabitants of the photic zone (nutrient poor) and hosting symbionts as their larger porcelaneous recent equivalents. They contrast with deeper water “lituolid” taxa and other deeper marine dwellers (hyaline perforate and planktonics r-strategists). They are narrowly linked to the carbonate platform history and evolution, birth and demise (correlated to paleotectonics or sea-level variations), and global climatic or volcanic events, OAE, etc.2.General principles used in evolutionary sciences can be applied to decipher some morphological pathways among foraminifera through time to reconstruct phylogenetical arborescences, e.g., embryology (heterochronies of development), recapitulation law (Haeckel), size increase (Deperet), parallel evolution, and biostratigraphy.3.Iterative evolution is the main mode of morphological variation through time and biostratigraphy helps to reconstruct the time repartition of diverging advanced homeomorphic taxa and their distinction. The new characters are issued from a constant, more tolerant stock of smaller and simpler primitive atavic forms by the transformation of previous structures or the addition of new ones. Advanced homeomorphic taxa are temporarily preserved and their morphological innovations linked probably to (epi)genetic constraints and symbiotic history increasing their energy efficiency in a rather stable (but cyclical) environment.4.Morphological innovations appear slowly during the Jurassic and more rapidly (and frequently) during the Cretaceous following a probable saltative and allopatric mode of evolution during favorable periods after main environmental crisis, anoxia, and sea-level changes. The Cretaceous is a time of great diversification (adaptive radiation of microgranular lituolids and larger porcelaneous tests).5.Morphological changes at a scale of one or two stages in one evolutive bioseries (general trend: size and internal complications increase) cannot be linked to global events or other abiotic factors (e.g., the orbitopsellids in the Pliensbachian) but are rather driven by internal epigenetic factors related to algal symbiosis and coevolution. The constancy of the model (text Fig. 8.2) through time in variable clades could be explained that way. The structural incompatibility between pseudokeriotheca/alveolae within the wall and marginal microstructures (radial partitions or hypodermic network) could be explained by a biological incompatibility of bacterial symbionts to live aside with larger microalgae as dinoflagellates. Local discontinuous events like cyclic (metric) parasequences are common on carbonate platforms but have no apparent influence on morphogenesis or population composition.6.Conversely, global environmental crises affect deeply the larger foraminifera (chiefly advanced larger tests) and population compositions at a higher taxonomic rank (families, etc.), replacing in the aftermath the larger solid tests by smaller forms with a fragile (thin) test during anoxic crisis (T/J—Late Pliensbachian—Late Cenomanian, etc.). Larger forms are too specialized and complicated in their architecture and are particularly sensitive to environmental changes (Hallock, Paleobiology 11(2):195–208, 1985). They cannot adapt their test morphology (“retrograde evolution,” Guex, Retrograde Evolution During Major Extinction Crisis, 2016) back to some kind of more tolerant simpler form because their low reproduction rates impede a rapid reaction to environmental stress, even for minor adjustments. Major sea-level and facies changes (deeper water conditions or large-scale emersions) cause the brutal disappearing of this very sensitive group of foraminifera. However, some large discoid taxa and other smaller siphovalvulinids-valvulinids cross the K/T environmental crisis, interpreted as survivors in the Paleocene.7.Moreover, gigantism is probably a disadvantage against physical perturbations like tidal currents and storms in an otherwise stable carbonate environment. In a first evolutionary step, increasing of test size and flattening of chambers are selective advantages in terms of energy (increasing of chemical exchanges with more symbionts) and stability on flat surfaces; but near the end of the evolutive bioseries, the same traits become a drawback concerning test anchorage and risk of displacement in unfavorable microenvironments." @default.
• W3044281872 created "2020-07-29" @default.
• W3044281872 creator A5048053436 @default.
• W3044281872 date "2020-01-01" @default.
• W3044281872 modified "2023-09-23" @default.
• W3044281872 title "Steps of Morphogenesis and Iterative Evolution of Imperforate Larger Foraminifera in Shallow Carbonate Shelves During Mesozoic Times: Possible Relations to Symbiotic and Abiotic Factors" @default.
• W3044281872 cites W1807528795 @default.
• W3044281872 cites W1830149513 @default.
• W3044281872 cites W1981979610 @default.
• W3044281872 cites W1997469183 @default.
• W3044281872 cites W2003194501 @default.
• W3044281872 cites W2014853842 @default.
• W3044281872 cites W2020795435 @default.
• W3044281872 cites W2020797827 @default.
• W3044281872 cites W2026004718 @default.
• W3044281872 cites W2029286475 @default.
• W3044281872 cites W2031696942 @default.
• W3044281872 cites W2046992166 @default.
• W3044281872 cites W2060681705 @default.
• W3044281872 cites W2078198550 @default.
• W3044281872 cites W2079852953 @default.
• W3044281872 cites W2082838582 @default.
• W3044281872 cites W2088801705 @default.
• W3044281872 cites W2105027613 @default.
• W3044281872 cites W2111194718 @default.
• W3044281872 cites W2122350895 @default.
• W3044281872 cites W2135970257 @default.
• W3044281872 cites W2170868235 @default.
• W3044281872 cites W2204470432 @default.
• W3044281872 cites W2289112191 @default.
• W3044281872 cites W2297718259 @default.
• W3044281872 cites W2312406830 @default.
• W3044281872 cites W2326669813 @default.
• W3044281872 cites W2337302658 @default.
• W3044281872 cites W2466813611 @default.
• W3044281872 cites W2482978179 @default.
• W3044281872 cites W2496651271 @default.
• W3044281872 cites W2500794243 @default.
• W3044281872 cites W2515142178 @default.
• W3044281872 cites W2736893197 @default.
• W3044281872 cites W2791620273 @default.
• W3044281872 cites W2892581091 @default.
• W3044281872 cites W2922719071 @default.
• W3044281872 cites W4244758974 @default.
• W3044281872 cites W4288852268 @default.
• W3044281872 cites W612211758 @default.
• W3044281872 doi "https://doi.org/10.1007/978-3-030-47279-5_8" @default.
• W3044281872 hasPublicationYear "2020" @default.
• W3044281872 type Work @default.
• W3044281872 sameAs 3044281872 @default.
• W3044281872 citedByCount "4" @default.
• W3044281872 countsByYear W30442818722021 @default.
• W3044281872 countsByYear W30442818722022 @default.
• W3044281872 countsByYear W30442818722023 @default.
• W3044281872 crossrefType "book-chapter" @default.
• W3044281872 hasAuthorship W3044281872A5048053436 @default.
• W3044281872 hasBestOaLocation W30442818722 @default.
• W3044281872 hasConcept C109007969 @default.
• W3044281872 hasConcept C111368507 @default.
• W3044281872 hasConcept C127313418 @default.
• W3044281872 hasConcept C132215390 @default.
• W3044281872 hasConcept C151730666 @default.
• W3044281872 hasConcept C178790620 @default.
• W3044281872 hasConcept C185592680 @default.
• W3044281872 hasConcept C202783661 @default.
• W3044281872 hasConcept C2780368712 @default.
• W3044281872 hasConcept C2780659211 @default.
• W3044281872 hasConcept C83042747 @default.
• W3044281872 hasConceptScore W3044281872C109007969 @default.
• W3044281872 hasConceptScore W3044281872C111368507 @default.
• W3044281872 hasConceptScore W3044281872C127313418 @default.
• W3044281872 hasConceptScore W3044281872C132215390 @default.
• W3044281872 hasConceptScore W3044281872C151730666 @default.
• W3044281872 hasConceptScore W3044281872C178790620 @default.
• W3044281872 hasConceptScore W3044281872C185592680 @default.
• W3044281872 hasConceptScore W3044281872C202783661 @default.
• W3044281872 hasConceptScore W3044281872C2780368712 @default.
• W3044281872 hasConceptScore W3044281872C2780659211 @default.
• W3044281872 hasConceptScore W3044281872C83042747 @default.
• W3044281872 hasLocation W30442818721 @default.
• W3044281872 hasLocation W30442818722 @default.
• W3044281872 hasLocation W30442818723 @default.
• W3044281872 hasOpenAccess W3044281872 @default.
• W3044281872 hasPrimaryLocation W30442818721 @default.
• W3044281872 hasRelatedWork W1970880851 @default.
• W3044281872 hasRelatedWork W2012750702 @default.
• W3044281872 hasRelatedWork W2022586609 @default.
• W3044281872 hasRelatedWork W2024259086 @default.
• W3044281872 hasRelatedWork W2268307399 @default.
• W3044281872 hasRelatedWork W2319379343 @default.
• W3044281872 hasRelatedWork W2319747825 @default.
• W3044281872 hasRelatedWork W2782780838 @default.
• W3044281872 hasRelatedWork W2909884302 @default.
• W3044281872 hasRelatedWork W4242594131 @default.
• W3044281872 isParatext "false" @default.
• W3044281872 isRetracted "false" @default.
• W3044281872 magId "3044281872" @default.
• W3044281872 workType "book-chapter" @default.