Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis
12 páginas.- 9 figuras.- 6 tablas.- 90 referencias
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2020 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/199494 |
| Acceso en línea: | http://hdl.handle.net/10261/199494 |
| Access Level: | acceso abierto |
| Palabra clave: | Flank margin caves Mixing dissolution Tides Bioconstruction-bioweathering processes |
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Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesisD’Angeli, Ilenia M.Naylor, L. A.Lee, MartinMiller, A. Z.Mylroie, JohnWaele, J. deFlank margin cavesMixing dissolutionTidesBioconstruction-bioweathering processes12 páginas.- 9 figuras.- 6 tablas.- 90 referenciasSan 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.the support from the CEECIND/01147/2017 contract funded by Fundação para a Ciência e a Tecnologia (Portugal). Funding was also provided by the Spanish project MINECO CGL2016-75590-P with ERDF funds.Peer reviewedElsevierFundação para a Ciência e a Tecnologia (Portugal)Ministerio de Economía, Industria y Competitividad (España)European CommissionD’Angeli, Ilenia M. [0000-0002-2471-62 36]Naylor, L. A. [0000-0002-4065-2674]Miller, A. Z. [0000-0002-0553-8470]Waele, J. de [0000-0001-5325-5208]Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202020202020info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/199494reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75590-Phttp://dx.doi.org/10.1016/j.geomorph.2020.107054Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1994942026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| title |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| spellingShingle |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis D’Angeli, Ilenia M. Flank margin caves Mixing dissolution Tides Bioconstruction-bioweathering processes |
| title_short |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| title_full |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| title_fullStr |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| title_full_unstemmed |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| title_sort |
Light attenuation as a control for microbiogeomorphic features: Implications for coastal cave speleogenesis |
| dc.creator.none.fl_str_mv |
D’Angeli, Ilenia M. Naylor, L. A. Lee, Martin Miller, A. Z. Mylroie, John Waele, J. de |
| author |
D’Angeli, Ilenia M. |
| author_facet |
D’Angeli, Ilenia M. Naylor, L. A. Lee, Martin Miller, A. Z. Mylroie, John Waele, J. de |
| author_role |
author |
| author2 |
Naylor, L. A. Lee, Martin Miller, A. Z. Mylroie, John Waele, J. de |
| author2_role |
author author author author author |
| dc.contributor.none.fl_str_mv |
Fundação para a Ciência e a Tecnologia (Portugal) Ministerio de Economía, Industria y Competitividad (España) European Commission D’Angeli, Ilenia M. [0000-0002-2471-62 36] Naylor, L. A. [0000-0002-4065-2674] Miller, A. Z. [0000-0002-0553-8470] Waele, J. de [0000-0001-5325-5208] Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Flank margin caves Mixing dissolution Tides Bioconstruction-bioweathering processes |
| topic |
Flank margin caves Mixing dissolution Tides Bioconstruction-bioweathering processes |
| description |
12 páginas.- 9 figuras.- 6 tablas.- 90 referencias |
| publishDate |
2020 |
| dc.date.none.fl_str_mv |
2020 2020 2020 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 Postprint info:eu-repo/semantics/acceptedVersion |
| format |
article |
| status_str |
acceptedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/199494 |
| url |
http://hdl.handle.net/10261/199494 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75590-P http://dx.doi.org/10.1016/j.geomorph.2020.107054 Sí |
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info:eu-repo/semantics/openAccess |
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openAccess |
| dc.publisher.none.fl_str_mv |
Elsevier |
| publisher.none.fl_str_mv |
Elsevier |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869420394915561472 |
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15,81155 |