FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015391105> ?p ?o ?g. }

• W2015391105 endingPage "258" @default.
• W2015391105 startingPage "241" @default.
• W2015391105 abstract "Dissolution experiments were carried out on a foraminiferal assemblage from the Paleocene–Eocene Thermal Maximum (PETM) at Dababiya, Egypt, in order to: 1) reveal the effects of differential dissolution on the composition of the foraminiferal assemblage and 2) develop objective criteria for the evaluation of dissolution in foraminiferal assemblages used in early Paleogene paleoenvironmental reconstructions, particularly with respect to neritic Midway-type assemblages from the Paleocene/Eocene transition. Our results confirm two general observations on modern foraminifera: 1) planktic foraminifera are much more vulnerable to dissolution than benthic foraminifera, leading to depressed P/B ratios and 2) dissolution susceptibility differs between size fractions, with the smaller specimens dissolving more rapidly than the bigger ones, leading to a larger average size of the remaining assemblage. Within a size fraction, wall structure and thickness are considered to be the main factors controlling differential dissolution susceptibility. We propose a ranking scheme for taxa with respect to dissolution resistance. Among the benthic taxa, Lenticulina is most resistant, followed by the agglutinated Gaudryina cf. ellisorae and Alabamina midwayensis. Biserial and triserial hyaline taxa and the porcelaneous Spiroloculina sp. are most susceptible to dissolution, whereas rotaliines, such as Cibicidoides and Anomalinoides have an intermediate susceptibility. This implies that mild dissolution of a Midway-type benthic assemblage leads to a relative enrichment in Lenticulina, Gaudryina and rotaliines. Amongst planktic foraminifera, the muricate taxa Acarinina and Morozovella are most resistant, followed by the cancellate Subbotina. The smooth and generally small Globanomalina and Zeauvigerina are least resistant to dissolution. Our data enable to objectively evaluate various degrees of dissolution in benthic and planktic foraminiferal assemblages retrieved from the lower Paleogene Tethyan outcrops. In this way taphonomic artifacts can be readily distinguished from paleoenvironmental signals affecting the primary composition of the assemblages. More generally, we propose that the combined use of foraminiferal numbers, P/B ratio and relative abundances of non-calcareous agglutinated taxa and Lenticulina may provide a powerful proxy for assessing dissolution in hemipelagic assemblages from Cenozoic and upper Cretaceous continental margins. In order to achieve more robust pre-Quaternary paleoenvironmental reconstructions based on quantitative foraminiferal data, application of dissolution proxies, like proposed here, or in slightly modified form, should become a more widely used micropaleontologic procedure. Particularly continental margin studies dealing with major biotic events (e.g. PETM) or employing P/B ratios for sea-level reconstructions should benefit from such an approach." @default.
• W2015391105 created "2016-06-24" @default.
• W2015391105 creator A5002194644 @default.
• W2015391105 creator A5013301552 @default.
• W2015391105 creator A5040587615 @default.
• W2015391105 date "2009-12-01" @default.
• W2015391105 modified "2023-10-10" @default.
• W2015391105 title "Experimental dissolution of a fossil foraminiferal assemblage (Paleocene–Eocene Thermal Maximum, Dababiya, Egypt): Implications for paleoenvironmental reconstructions" @default.
• W2015391105 cites W1978530965 @default.
• W2015391105 cites W1983686809 @default.
• W2015391105 cites W1985282541 @default.
• W2015391105 cites W1985964613 @default.
• W2015391105 cites W1986077000 @default.
• W2015391105 cites W1990366259 @default.
• W2015391105 cites W1994025151 @default.
• W2015391105 cites W1994271054 @default.
• W2015391105 cites W1999638079 @default.
• W2015391105 cites W2000349058 @default.
• W2015391105 cites W2003806399 @default.
• W2015391105 cites W2011270134 @default.
• W2015391105 cites W2011752333 @default.
• W2015391105 cites W2014518530 @default.
• W2015391105 cites W2015224563 @default.
• W2015391105 cites W2015796175 @default.
• W2015391105 cites W2016225258 @default.
• W2015391105 cites W2019600437 @default.
• W2015391105 cites W2028679627 @default.
• W2015391105 cites W2029620213 @default.
• W2015391105 cites W2030891075 @default.
• W2015391105 cites W2036774334 @default.
• W2015391105 cites W2037850111 @default.
• W2015391105 cites W2038977064 @default.
• W2015391105 cites W2040550239 @default.
• W2015391105 cites W2045242213 @default.
• W2015391105 cites W2045496658 @default.
• W2015391105 cites W2046771951 @default.
• W2015391105 cites W2054014497 @default.
• W2015391105 cites W2056692175 @default.
• W2015391105 cites W2058938294 @default.
• W2015391105 cites W2061866583 @default.
• W2015391105 cites W2066287721 @default.
• W2015391105 cites W2073410689 @default.
• W2015391105 cites W2077441776 @default.
• W2015391105 cites W2077651183 @default.
• W2015391105 cites W2079975199 @default.
• W2015391105 cites W2083084875 @default.
• W2015391105 cites W2083943234 @default.
• W2015391105 cites W2084688963 @default.
• W2015391105 cites W2088880599 @default.
• W2015391105 cites W2096688606 @default.
• W2015391105 cites W2100500003 @default.
• W2015391105 cites W2120666502 @default.
• W2015391105 cites W2127316389 @default.
• W2015391105 cites W2129224463 @default.
• W2015391105 cites W2145527576 @default.
• W2015391105 cites W2157438953 @default.
• W2015391105 cites W2167650831 @default.
• W2015391105 cites W2171357973 @default.
• W2015391105 cites W2185985925 @default.
• W2015391105 cites W2313761502 @default.
• W2015391105 cites W2328166471 @default.
• W2015391105 cites W2328519808 @default.
• W2015391105 cites W2481564683 @default.
• W2015391105 cites W4251295027 @default.
• W2015391105 doi "https://doi.org/10.1016/j.marmicro.2009.10.005" @default.
• W2015391105 hasPublicationYear "2009" @default.
• W2015391105 type Work @default.
• W2015391105 sameAs 2015391105 @default.
• W2015391105 citedByCount "63" @default.
• W2015391105 countsByYear W20153911052012 @default.
• W2015391105 countsByYear W20153911052013 @default.
• W2015391105 countsByYear W20153911052014 @default.
• W2015391105 countsByYear W20153911052015 @default.
• W2015391105 countsByYear W20153911052016 @default.
• W2015391105 countsByYear W20153911052017 @default.
• W2015391105 countsByYear W20153911052018 @default.
• W2015391105 countsByYear W20153911052019 @default.
• W2015391105 countsByYear W20153911052020 @default.
• W2015391105 countsByYear W20153911052021 @default.
• W2015391105 countsByYear W20153911052022 @default.
• W2015391105 countsByYear W20153911052023 @default.
• W2015391105 crossrefType "journal-article" @default.
• W2015391105 hasAuthorship W2015391105A5002194644 @default.
• W2015391105 hasAuthorship W2015391105A5013301552 @default.
• W2015391105 hasAuthorship W2015391105A5040587615 @default.
• W2015391105 hasBestOaLocation W20153911052 @default.
• W2015391105 hasConcept C109007969 @default.
• W2015391105 hasConcept C111368507 @default.
• W2015391105 hasConcept C127313418 @default.
• W2015391105 hasConcept C147789679 @default.
• W2015391105 hasConcept C151730666 @default.
• W2015391105 hasConcept C185592680 @default.
• W2015391105 hasConcept C204330871 @default.
• W2015391105 hasConcept C2777798969 @default.
• W2015391105 hasConcept C2780368712 @default.
• W2015391105 hasConcept C71640776 @default.
• W2015391105 hasConcept C83042747 @default.
• W2015391105 hasConcept C88380143 @default.

• next