Underwater optics in sub-antarctic and antarctic coastal ecosystems

dc.contributor.authorHuovinen, Pirjo
dc.contributor.authorRamírez, Jaime
dc.contributor.authorGómez, Iván
dc.contributor.editorBan, Syuhei
dc.date.accessioned2019-01-04T13:45:18Z
dc.date.available2019-01-04T13:45:18Z
dc.date.issued2016-05-04
dc.description.abstractUnderstanding underwater optics in natural waters is essential in evaluating aquatic primary production and risk of UV exposure in aquatic habitats. Changing environmental conditions related with global climate change, which imply potential contrasting changes in underwater light climate further emphasize the need to gain insights into patterns related with underwater optics for more accurate future predictions. The present study evaluated penetration of solar radiation in six sub-Antarctic estuaries and fjords in Chilean North Patagonian region (39-44 degrees S) and in an Antarctic bay (62 degrees S). Based on vertical diffuse attenuation coefficients (K-d), derived from measurements with a submersible multichannel radiometer, average summer UV penetration depth (z(1%)) in these water bodies ranged 2-11 m for UV-B (313 nm), 4-27 m for UV-A (395 nm), and 7-30 m for PAR (euphotic zone). UV attenuation was strongest in the shallow Quempillen estuary, while Fildes Bay (Antarctica) exhibited the highest transparency. Optically non-homogeneous water layers and seasonal variation in transparency (lower in winter) characterized Comau Fjord and Puyuhuapi Channel. In general, multivariate analysis based on K-d values of UV and PAR wavelengths discriminated strongly Quempillen estuary and Puyuhuapi Channel from other study sites. Spatial (horizontal) variation within the estuary of Valdivia river reflected stronger attenuation in zones receiving river impact, while within Fildes Bay a lower spatial variation in water transparency could in general be related to closeness of glaciers, likely due to increased turbidity through ice-driven processes. Higher transparency and deeper UV-B penetration in proportion to UV-A/visible wavelengths observed in Fildes Bay suggests a higher risk for Antarctic ecosystems reflected by e.g. altered UV-B damage vs. photorepair under UV-A/PAR. Considering that damage repair processes often slow down under cool temperatures, adverse UV impact could be further exacerbated by cold temperatures in this location, together with episodes of ozone depletion. Overall, the results emphasize the marked spatial (horizontal and vertical) and temporal heterogeneity of optical characteristics, and challenges that these imply for estimations of underwater optics.es_ES
dc.description.sponsorshipFondo Nacional de Desarrollo Cientifico y Tecnologico (FONDECYT-CONICYT) 1130582 1130794 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) Anillo ART1101 Centro Fondap-IDEAL (Grant 15150003es_ES
dc.identifier.citationPLoS ONE 11(5): e0154887es_ES
dc.identifier.issn1932-6203
dc.identifier.otherdoi:10.1371/journal.pone.0154887
dc.identifier.urihttp://hdl.handle.net/20.500.11894/1209
dc.language.isoenes_ES
dc.publisherPublic Library of Science (PLOS)es_ES
dc.relation.ispartofPlos Onees_ES
dc.relation.ispartofVol. 11(5)
dc.rightsCreative Commons Attribution 4.0 International licensees_ES
dc.subjectCienciaes_ES
dc.subjectSolar ultraviolet radiationes_ES
dc.subjectUV-B radiationes_ES
dc.subjectOzone depletiones_ES
dc.titleUnderwater optics in sub-antarctic and antarctic coastal ecosystemses_ES
dc.typeArtículoes_ES

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