FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2310607180> ?p ?o ?g. }

• W2310607180 endingPage "85" @default.
• W2310607180 startingPage "69" @default.
• W2310607180 abstract "New hydroacoustic data, high resolution multichannel seismic reflection data, CTD casts and sampling document the dominance of bottom currents and the occurrence of carbonate mounds in the Santaren Channel off Great Bahama Bank and Cay Sal Bank. Based on these data sets, three types of carbonate mounds have been identified in water depths between 285 and 685 m. Their distribution is strongly related to the present current regime. Bank-driven sediments are caught up by the currents and redeposited mainly in the channel center, resulting in the accumulation of giant confined drifts flanked by moats. The moats at the banks toe-of-slope are formed by a southward and northward flowing water mass, respectively, mainly Antarctic Intermediate Water and Subtropical Underwater. The observed carbonate mounds are concentrated in these moats. Mound type 1 has an elongated shape parallel to the prevailing bottom current direction, a gently inclined flank facing the water flow and a steep flank in its current shadow. Its upstream flank is covered by a thin sediment wedge whereas the lee side is marked by a parabolic scour. Type 1 occurs at both bank margins but mainly off Great Bahama Bank, consisting of cold-water coral rubble floating in a sediment matrix and is, thus, interpreted as cold-water coral mound. By contrast, type 2 mounds are restricted to the Cay Sal margin and have a predominately conical outline. Bottom samples including living sessile crinoids show that its surface must be lithified and colonized by macroepibenthos, except corals. The mounds are situated in pockmark-like depressions that are underlain by fluid escape structures like pipes and chimneys. These fluid pathways are generated by a network of fractures. Mound type 2 is probably formed by abiotic carbonate precipitation; however, a chemoherm nature cannot be ruled out. Mound type 3 has a conical to polygonal shape and occurs off Cay Sal Bank and Great Bahama Bank. It is surrounded by a scour which is elongated in downcurrent and crescent in upcurrent direction. A sediment bulge formed at its front. This type is consistent with blocks and boulders colonized by macroepibenthos and related to gravity-controlled mass movements at the steep bank slopes. Principally, two habitats can be distinguished: the Great Bahama Bank periplatform deep-water province dominated by mound type 1 and the Cay Sal Bank slope to basin province occupied by mound type 2 that is associated with pockmark-like structures. Mound type 3 occurs in both habitats. Physical water mass properties for the existence of cold-water corals are limited to a depth range of ca. 430 to 685 m, with seawater densities (σ-θ) of 26.93 to 27.29 kg/m and temperatures below 13 °C. Their dominance off Great Bahama Bank might be addressed to a more effective food supply induced by local downwelling." @default.
• W2310607180 created "2016-06-24" @default.
• W2310607180 creator A5003083523 @default.
• W2310607180 creator A5018274268 @default.
• W2310607180 creator A5027648877 @default.
• W2310607180 creator A5030083359 @default.
• W2310607180 creator A5045536244 @default.
• W2310607180 creator A5079590755 @default.
• W2310607180 creator A5069864342 @default.
• W2310607180 date "2016-06-01" @default.
• W2310607180 modified "2023-10-02" @default.
• W2310607180 title "Carbonate mounds in the Santaren Channel, Bahamas: A current-dominated periplatform depositional regime" @default.
• W2310607180 cites W1565924741 @default.
• W2310607180 cites W1604851612 @default.
• W2310607180 cites W174503446 @default.
• W2310607180 cites W1874516583 @default.
• W2310607180 cites W1964619074 @default.
• W2310607180 cites W1964927832 @default.
• W2310607180 cites W1966614422 @default.
• W2310607180 cites W1968338161 @default.
• W2310607180 cites W1969288612 @default.
• W2310607180 cites W1975973488 @default.
• W2310607180 cites W1976739569 @default.
• W2310607180 cites W1977518148 @default.
• W2310607180 cites W1982848394 @default.
• W2310607180 cites W1985882235 @default.
• W2310607180 cites W1987204045 @default.
• W2310607180 cites W1991869233 @default.
• W2310607180 cites W1995847317 @default.
• W2310607180 cites W1998561141 @default.
• W2310607180 cites W2010420808 @default.
• W2310607180 cites W2013328420 @default.
• W2310607180 cites W2018196236 @default.
• W2310607180 cites W2021729345 @default.
• W2310607180 cites W2024694523 @default.
• W2310607180 cites W2028292727 @default.
• W2310607180 cites W2028545220 @default.
• W2310607180 cites W2028589282 @default.
• W2310607180 cites W2032266557 @default.
• W2310607180 cites W2033119977 @default.
• W2310607180 cites W2035006759 @default.
• W2310607180 cites W2035458263 @default.
• W2310607180 cites W2046091863 @default.
• W2310607180 cites W2050111640 @default.
• W2310607180 cites W2054149374 @default.
• W2310607180 cites W2056331609 @default.
• W2310607180 cites W2063017655 @default.
• W2310607180 cites W2064400126 @default.
• W2310607180 cites W2064707991 @default.
• W2310607180 cites W2065089649 @default.
• W2310607180 cites W2067946096 @default.
• W2310607180 cites W2069989223 @default.
• W2310607180 cites W2070289546 @default.
• W2310607180 cites W2077250325 @default.
• W2310607180 cites W2083415053 @default.
• W2310607180 cites W2083585274 @default.
• W2310607180 cites W2089358284 @default.
• W2310607180 cites W2093879665 @default.
• W2310607180 cites W2103048256 @default.
• W2310607180 cites W2104528633 @default.
• W2310607180 cites W2105808087 @default.
• W2310607180 cites W2112902763 @default.
• W2310607180 cites W2114227729 @default.
• W2310607180 cites W2121800158 @default.
• W2310607180 cites W2136533606 @default.
• W2310607180 cites W2137258492 @default.
• W2310607180 cites W2145619152 @default.
• W2310607180 cites W2172106945 @default.
• W2310607180 cites W2323615192 @default.
• W2310607180 cites W2327801799 @default.
• W2310607180 doi "https://doi.org/10.1016/j.margeo.2016.03.013" @default.
• W2310607180 hasPublicationYear "2016" @default.
• W2310607180 type Work @default.
• W2310607180 sameAs 2310607180 @default.
• W2310607180 citedByCount "30" @default.
• W2310607180 countsByYear W23106071802016 @default.
• W2310607180 countsByYear W23106071802017 @default.
• W2310607180 countsByYear W23106071802018 @default.
• W2310607180 countsByYear W23106071802019 @default.
• W2310607180 countsByYear W23106071802020 @default.
• W2310607180 countsByYear W23106071802021 @default.
• W2310607180 countsByYear W23106071802022 @default.
• W2310607180 countsByYear W23106071802023 @default.
• W2310607180 crossrefType "journal-article" @default.
• W2310607180 hasAuthorship W2310607180A5003083523 @default.
• W2310607180 hasAuthorship W2310607180A5018274268 @default.
• W2310607180 hasAuthorship W2310607180A5027648877 @default.
• W2310607180 hasAuthorship W2310607180A5030083359 @default.
• W2310607180 hasAuthorship W2310607180A5045536244 @default.
• W2310607180 hasAuthorship W2310607180A5069864342 @default.
• W2310607180 hasAuthorship W2310607180A5079590755 @default.
• W2310607180 hasConcept C109007969 @default.
• W2310607180 hasConcept C111368507 @default.
• W2310607180 hasConcept C114793014 @default.
• W2310607180 hasConcept C126753816 @default.
• W2310607180 hasConcept C127313418 @default.
• W2310607180 hasConcept C140302290 @default.
• W2310607180 hasConcept C143020374 @default.

• next