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dc.contributor.authorPicard, Kim  Concept link
dc.contributor.authorBrooke, Brendan P.  Concept link
dc.contributor.authorHarris, Peter T.  Concept link
dc.contributor.authorSiwabessy, Paulus J. W.  Concept link
dc.contributor.authorCoffin, Millard F.  Concept link
dc.contributor.authorTran, Maggie  Concept link
dc.contributor.authorSpinoccia, Michele  Concept link
dc.contributor.authorWeales, Jonathan  Concept link
dc.contributor.authorMacmillan-Lawler, Miles  Concept link
dc.contributor.authorSullivan, Jonah  Concept link
dc.date.accessioned2018-02-16T16:59:41Z
dc.date.available2018-02-16T16:59:41Z
dc.date.issued2017-11-08
dc.identifier.citationMarine Geology 395 (2018): 301-319en_US
dc.identifier.urihttps://hdl.handle.net/1912/9589
dc.description© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Marine Geology 395 (2018): 301-319, doi:10.1016/j.margeo.2017.10.014.en_US
dc.description.abstractA high-resolution multibeam echosounder (MBES) dataset covering over 279,000 km2 was acquired in the southeastern Indian Ocean to assist the search for Malaysia Airlines Flight 370 (MH370) that disappeared on 8 March 2014. The data provided an essential geospatial framework for the search and is the first large-scale coverage of MBES data in this region. Here we report on geomorphic analyses of the new MBES data, including a comparison with the Global Seafloor Geomorphic Features Map (GSFM) that is based on coarser resolution satellite altimetry data, and the insights the new data provide into geological processes that have formed and are currently shaping this remote deepsea area. Our comparison between the new MBES bathymetric model and the latest global topographic/bathymetric model (SRTM15_plus) reveals that 62% of the satellite-derived data points for the study area are comparable with MBES measurements within the estimated vertical uncertainty of the SRTM15_plus model (± 100 m). However, > 38% of the SRTM15_plus depth estimates disagree with the MBES data by > 100 m, in places by up to 1900 m. The new MBES data show that abyssal plains and basins in the study area are significantly more rugged than their representation in the GSFM, with a 20% increase in the extent of hills and mountains. The new model also reveals four times more seamounts than presented in the GSFM, suggesting more of these features than previously estimated for the broader region. This is important considering the ecological significance of high-relief structures on the seabed, such as hosting high levels of biodiversity. Analyses of the new data also enabled sea knolls, fans, valleys, canyons, troughs, and holes to be identified, doubling the number of discrete features mapped. Importantly, mapping the study area using MBES data improves our understanding of the geological evolution of the region and reveals a range of modern sedimentary processes. For example, a large series of ridges extending over approximately 20% of the mapped area, in places capped by sea knolls, highlight the preserved seafloor spreading fabric and provide valuable insights into Southeast Indian Ridge seafloor spreading processes, especially volcanism. Rifting is also recorded along the Broken Ridge – Diamantina Escarpment, with rift blocks and well-bedded sedimentary bedrock outcrops discernible down to 2400 m water depth. Modern ocean floor sedimentary processes are documented by sediment mass transport features, especially along the northern margin of Broken Ridge, and in pockmarks (the finest-scale features mapped), which are numerous south of Diamantina Trench and appear to record gas and/or fluid discharge from underlying marine sediments. The new MBES data highlight the complexity of the search area and serve to demonstrate how little we know about the vast areas of the ocean that have not been mapped with MBES. The availability of high-resolution and accurate maps of the ocean floor can clearly provide new insights into the Earth's geological evolution, modern ocean floor processes, and the location of sites that are likely to have relatively high biodiversity.en_US
dc.language.isoen_USen_US
dc.publisherElsevieren_US
dc.relation.urihttps://doi.org/10.1016/j.margeo.2017.10.014
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectIndian Oceanen_US
dc.subjectMultibeam echosounderen_US
dc.subjectGeomorphologyen_US
dc.subjectProcessesen_US
dc.subjectDeepseaen_US
dc.subjectSeamounten_US
dc.titleMalaysia Airlines flight MH370 search data reveal geomorphology and seafloor processes in the remote southeast Indian Oceanen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.margeo.2017.10.014


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International