Claire L. Mellett

ORCID: 0000-0003-0865-1513
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About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Geological formations and processes
  • Methane Hydrates and Related Phenomena
  • Planetary Science and Exploration
  • Geological and Geophysical Studies
  • Coastal wetland ecosystem dynamics
  • Marine and environmental studies
  • Astro and Planetary Science
  • Paleontology and Stratigraphy of Fossils
  • Maritime and Coastal Archaeology
  • Coastal and Marine Dynamics
  • Geomagnetism and Paleomagnetism Studies
  • Seismic Imaging and Inversion Techniques
  • Geological and Geochemical Analysis
  • Cryospheric studies and observations
  • Pleistocene-Era Hominins and Archaeology
  • Archaeology and ancient environmental studies
  • Hydrology and Sediment Transport Processes
  • Underwater Acoustics Research
  • Hydrocarbon exploration and reservoir analysis
  • Space Exploration and Technology
  • Oceanographic and Atmospheric Processes
  • Aeolian processes and effects
  • Evolution and Paleontology Studies
  • Soil erosion and sediment transport

Royal HaskoningDHV (United Kingdom)
2024

University of Leeds
2024

British Geological Survey
2014-2019

Heriot-Watt University
2019

Salisbury District Hospital
2018

Continental (Canada)
2017

International Ocean Discovery Program
2017

University of Liverpool
2012-2013

Drilling into Chicxulub's formation The Chicxulub impact crater, known for its link to the demise of dinosaurs, also provides an opportunity study rocks from a large structure. Large craters have “peak rings” that define complex crater morphology. Morgan et al. looked at drilling expedition through peak rings (see Perspective by Barton). drill cores features consistent with model postulates single over-heightened central collapsed multiple-peak-ring validity this has implications far-ranging...

10.1126/science.aah6561 article EN Science 2016-11-17

Abstract For a long time global paleodust numerical simulations have greatly underestimated dust sources other than modern deserts. Recent modeling experiments incorporating glaciogenic of positively improved the agreement between model and data. This highlights importance accurately representing all areas potentially subjected to deflation during an investigated interval. Geochemical results, obtained from European loess sequences collected along 50°N transect, combined with emission reveal...

10.1002/2014gl061382 article EN Geophysical Research Letters 2014-10-01

The erosional morphology preserved at the sea bed in eastern English Channel dominantly records denudation of continental shelf by fluvial processes over multiple glacial-interglacial sea-level cycles rather than catastrophic flooding through Straits Dover during mid-Quaternary. Here, integration multibeam bathymetry and shallow sub-bottom 2D seismic reflection profiles calibrated with vibrocore records, first stratigraphic model erosion deposition on is presented. Published Optical...

10.1016/j.geomorph.2013.03.030 article EN cc-by Geomorphology 2013-04-08

The Celtic Sea contains the world's largest continental shelf sediment ridges. These megaridges were initially interpreted as tidal features formed during post-glacial marine transgression, but glacigenic sediments have been recovered from their flanks. We examine stratigraphy of using new decimetric-resolution geophysical data correlated to cores test hypothetical vs glacial modes formation. comprise three main units, 1) a superficial fining-upward drape that extends across above an...

10.1016/j.quascirev.2018.08.029 article EN cc-by Quaternary Science Reviews 2018-09-10

High‐resolution shallow sub‐bottom seismic survey data obtained for the Dudgeon windfarm site located 50 km offshore of north Norfolk coast in southern North Sea have revealed that chalk bedrock this area is overlain by sediments deposited during Elsterian and Weichselian glacial periods. A buried N–S‐trending subglacial drainage channel (tunnel valley) filled with Swarte Bank Formation ( MIS 12) indicates maximum extent ice‐sheet margin occurred further to south. Detailed cross‐sections...

10.1111/bor.12410 article EN Boreas 2019-10-17

ABSTRACT Offshore stratigraphic records from the North Sea contain information to reconstruct palaeo‐ice‐sheet extent and understand sedimentary processes landscape response Pleistocene glacial–interglacial cycles. We document three major Middle Late packages over a 401‐km 2 area (Norfolk Vanguard/Boreas Wind Farm), offshore East Anglia, UK, through integration of 2D seismic, borehole cone penetration test data. The lowermost unit is predominantly fluviatile [Yarmouth Roads Formation, Marine...

10.1002/jqs.3230 article EN cc-by Journal of Quaternary Science 2020-07-13

Abstract. Submerged landscapes on continental shelves archive drainage networks formed during periods of sea-level lowstand. The evolution these postglacial also reveals how past climate changes affected the landscape. Ice-marginal and paraglacial low-relief topography are susceptible to reorganisation water supply, forced by ice-marginal rearrangement, precipitation temperature variations, marine inundation. A rare geological climate-driven landscape transition from (ca. 23 ka) a fully...

10.5194/esurf-8-869-2020 article EN cc-by Earth Surface Dynamics 2020-10-23

ABSTRACT Mesolithic settlement sites preserved on the north‐east coast of England and in south‐east Scotland drive questions about relationship between early human Holocene palaeogeography ‘Doggerland’. Palaeogeographical reconstructions before 8000 years ago have been restricted by a lack sea‐level index points particularly sparse nearshore geophysical geological datasets required for such reconstructions. This paper presents new high‐resolution survey data from Northumberland's ‘white...

10.1002/jqs.2897 article EN Journal of Quaternary Science 2016-12-07

Abstract Low‐relief coastal landscapes are at major risk of rising sea levels, as vertical changes in relative level have far‐reaching lateral effects. Integration a dense 2D grid seismic reflection data with sedimentological and geotechnical obtained two offshore wind farm zones allows detailed documentation postglacial landforms environmental change over 1,021 km 2 area the western sector southern North Sea. Following retreat Last Glacial Maximum ice sheets from Sea, resulting terrestrial...

10.1002/esp.5880 article EN cc-by Earth Surface Processes and Landforms 2024-05-15

Abstract. Expedition 364 was a joint IODP and ICDP mission-specific platform (MSP) expedition to explore the Chicxulub impact crater buried below surface of Yucatán continental shelf seafloor. In April May 2016, this drilled single borehole at Site M0077 into crater's peak ring. Excellent quality cores were recovered from ∼505 ∼1335 m seafloor (m b.s.f.), high-resolution open hole logs acquired between total drill depth. Downhole are used image wall, measure physical properties rocks that...

10.5194/sd-24-1-2018 article EN cc-by Scientific Drilling 2018-10-22
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