FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3001077067> ?p ?o ?g. }

• W3001077067 endingPage "107054" @default.
• W3001077067 startingPage "107054" @default.
• W3001077067 abstract "San Salvador (Bahamas) is a carbonate island with dozens of flank margin caves formed in the phreatic zone by fresh seawater mixing within the freshwater lens. These caves have no direct connection with the sea, and form at or close to the tidally influenced fluctuating water table. After sea-level fall, in their subaerial parts caves are enlarged mainly by rock dissolution and by erosion close to the water level, condensation-corrosion and breakdown processes. For understanding the geomorphological features observed in these caves and how they are related to light attenuation, we investigated three sampling sites in the tidally influenced zone of Lighthouse Cave, which has been re-invaded by seawater during the Holocene sea-level highstand. A freshwater lens no longer exists within or adjacent to the cave. Rock samples were collected above and below the internal lake shores close to the entrance, and in the twilight and dark zones of this cave. Light and electron microscopy examinations were conducted for detecting microbial cells, as well as bioconstruction and bioweathering features. In addition, a high precision laser scanner was used for characterising sample microtopography. Our data showed that the microtopography and geomorphology of the lake shore samples (cave entrance) are dominated by bioweathering, whereas the samples of the twilight and dark zones are controlled by a combination of both bioweathering and bioconstructive processes depending on light availability. Bioconstructive structures, such as semi-planar lamination, at the fluctuating water level of the Lighthouse Cave show that dissolution due to water mixing of sea and freshwater in the Holocene is no longer the most important speleogenetic process. We propose that the geomorphological evolution is strongly influenced by the degree of rock diagenesis more than the initial mechanism of speleogenesis." @default.
• W3001077067 created "2020-01-30" @default.
• W3001077067 creator A5022780531 @default.
• W3001077067 creator A5029188869 @default.
• W3001077067 creator A5077403897 @default.
• W3001077067 creator A5084170385 @default.
• W3001077067 creator A5085965513 @default.
• W3001077067 creator A5087216556 @default.
• W3001077067 date "2020-04-01" @default.
• W3001077067 modified "2023-09-24" @default.
• W3001077067 title "Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis" @default.
• W3001077067 cites W1555119012 @default.
• W3001077067 cites W1746567743 @default.
• W3001077067 cites W1940385015 @default.
• W3001077067 cites W1966041810 @default.
• W3001077067 cites W1973250277 @default.
• W3001077067 cites W1973608910 @default.
• W3001077067 cites W1975176385 @default.
• W3001077067 cites W1978264842 @default.
• W3001077067 cites W1980873543 @default.
• W3001077067 cites W1984221800 @default.
• W3001077067 cites W1988820190 @default.
• W3001077067 cites W1994000181 @default.
• W3001077067 cites W1998773304 @default.
• W3001077067 cites W1998837502 @default.
• W3001077067 cites W1999095249 @default.
• W3001077067 cites W2000964854 @default.
• W3001077067 cites W2009186438 @default.
• W3001077067 cites W2010427711 @default.
• W3001077067 cites W2016888144 @default.
• W3001077067 cites W2023195805 @default.
• W3001077067 cites W2033410553 @default.
• W3001077067 cites W2037197962 @default.
• W3001077067 cites W2037761303 @default.
• W3001077067 cites W2045413544 @default.
• W3001077067 cites W2046352429 @default.
• W3001077067 cites W2052967611 @default.
• W3001077067 cites W2060140623 @default.
• W3001077067 cites W2060289601 @default.
• W3001077067 cites W2070545235 @default.
• W3001077067 cites W2070678064 @default.
• W3001077067 cites W2080897878 @default.
• W3001077067 cites W2081805883 @default.
• W3001077067 cites W2082432227 @default.
• W3001077067 cites W2086766693 @default.
• W3001077067 cites W2092948336 @default.
• W3001077067 cites W2107030413 @default.
• W3001077067 cites W2113100380 @default.
• W3001077067 cites W2113162904 @default.
• W3001077067 cites W2114259874 @default.
• W3001077067 cites W2121255959 @default.
• W3001077067 cites W2121879569 @default.
• W3001077067 cites W2123502054 @default.
• W3001077067 cites W2135429048 @default.
• W3001077067 cites W2150231600 @default.
• W3001077067 cites W2153175030 @default.
• W3001077067 cites W2162034920 @default.
• W3001077067 cites W2172040928 @default.
• W3001077067 cites W2193444923 @default.
• W3001077067 cites W2252713149 @default.
• W3001077067 cites W2259939606 @default.
• W3001077067 cites W2317892175 @default.
• W3001077067 cites W2338877333 @default.
• W3001077067 cites W2344526629 @default.
• W3001077067 cites W2407616959 @default.
• W3001077067 cites W2565302098 @default.
• W3001077067 cites W2765843185 @default.
• W3001077067 cites W2778269921 @default.
• W3001077067 cites W2794619777 @default.
• W3001077067 cites W2915307253 @default.
• W3001077067 cites W2942034432 @default.
• W3001077067 doi "https://doi.org/10.1016/j.geomorph.2020.107054" @default.
• W3001077067 hasPublicationYear "2020" @default.
• W3001077067 type Work @default.
• W3001077067 sameAs 3001077067 @default.
• W3001077067 citedByCount "2" @default.
• W3001077067 countsByYear W30010770672021 @default.
• W3001077067 countsByYear W30010770672022 @default.
• W3001077067 crossrefType "journal-article" @default.
• W3001077067 hasAuthorship W3001077067A5022780531 @default.
• W3001077067 hasAuthorship W3001077067A5029188869 @default.
• W3001077067 hasAuthorship W3001077067A5077403897 @default.
• W3001077067 hasAuthorship W3001077067A5084170385 @default.
• W3001077067 hasAuthorship W3001077067A5085965513 @default.
• W3001077067 hasAuthorship W3001077067A5087216556 @default.
• W3001077067 hasBestOaLocation W30010770672 @default.
• W3001077067 hasConcept C114793014 @default.
• W3001077067 hasConcept C120665830 @default.
• W3001077067 hasConcept C121332964 @default.
• W3001077067 hasConcept C127313418 @default.
• W3001077067 hasConcept C151730666 @default.
• W3001077067 hasConcept C166957645 @default.
• W3001077067 hasConcept C171878925 @default.
• W3001077067 hasConcept C184652730 @default.
• W3001077067 hasConcept C205649164 @default.
• W3001077067 hasConceptScore W3001077067C114793014 @default.
• W3001077067 hasConceptScore W3001077067C120665830 @default.
• W3001077067 hasConceptScore W3001077067C121332964 @default.

• next