Universität zu Köln

May, Simon Matthias ORCID: 0000-0001-6762-7500, Gelhausen, Henrik, Brill, Dominik ORCID: 0000-0001-8637-4641, Callow, John Nikolaus, Engel, Max ORCID: 0000-0002-2271-4229, Opitz, Stephan, Scheffers, Anja ORCID: 0000-0002-9143-5389, Joannes-Boyau, Renaud ORCID: 0000-0002-0452-486X, Leopold, Matthias ORCID: 0000-0003-0716-0093 and Brueckner, Helmut (2018). Chenier-type ridges in Giralia Bay (Exmouth Gulf, Western Australia) - Processes, chronostratigraphy, and significance for recording past tropical cyclones. Mar. Geol., 396. S. 186 - 205. AMSTERDAM: ELSEVIER SCIENCE BV. ISSN 1872-6151

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Abstract

Past coastal flooding events may be inferred from geomorphic and sedimentary archives, including particular landforms (e.g., beach ridges, washover fans), deposits (e.g., washover sediments in lagoons) or erosional features (e.g., erosional scarps within strandplains). In Giralia Bay, southern Exmouth Gulf (Western Australia), sandy ridge sequences in supratidal elevations form the landward margin of extensive mudflats. The formation of these ridges is assumed to be mainly driven by tropical cyclones (TCs), although their depositional processes need to be clarified. We investigated the supratidal sandy ridge sequence in Giralia Bay by carrying out process monitoring, geomorphological mapping by means of an unmanned aerial vehicle survey, as well as sedimentological and geochronological investigations and multivariate statistics. Based on the resulting data, this study aims at (i) identifying the most important driving processes to form the sandy ridges; (ii) establishing their chronostratigraphy; and (iii) understanding their significance for recording past TC activity. Trench excavations revealed sandy units that are interbedded with mud layers at the base, similar to the present distal mudflat sediments. On top, mud intercalations recede, and sand layers of varying grain size distribution dominate. In the upper part of the trenches, younger sediment layers onlap older ones documenting the stepwise seaward accretion of the ridges onto the mudflat While our data suggests that tidal processes have only limited effects on ridge activity, sediment transport, erosion and deposition seems to be driven by both TC-induced storm surges and high magnitude precipitation events causing surface discharge. Most accretionary sand units are thus assumed to represent events of morphodynamic activity during TC-induced flooding since the mid-Holocene. Ridge activity is recorded in a roughly decadal resolution and over historical as well as prehistorical/Holocene time scales. While the ridges do not represent beach or chenier ridges sensu stricto, they may be described as chenier-type ridges due to their stratigraphical architecture. Ridge evolution, however, over a millennial time scale seems to be indicated by the landward rise of the sequence possibly corresponding to the mid-Holocene sea-level highstand of Western Australia of at least 1-2 m above present mean sea level. (C) 2017 Elsevier B.V. All rights reserved.

Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code May, Simon Matthias UNSPECIFIED orcid.org/0000-0001-6762-7500 UNSPECIFIED Gelhausen, Henrik UNSPECIFIED UNSPECIFIED UNSPECIFIED Brill, Dominik UNSPECIFIED orcid.org/0000-0001-8637-4641 UNSPECIFIED Callow, John Nikolaus UNSPECIFIED UNSPECIFIED UNSPECIFIED Engel, Max UNSPECIFIED orcid.org/0000-0002-2271-4229 UNSPECIFIED Opitz, Stephan UNSPECIFIED UNSPECIFIED UNSPECIFIED Scheffers, Anja UNSPECIFIED orcid.org/0000-0002-9143-5389 UNSPECIFIED Joannes-Boyau, Renaud UNSPECIFIED orcid.org/0000-0002-0452-486X UNSPECIFIED Leopold, Matthias UNSPECIFIED orcid.org/0000-0003-0716-0093 UNSPECIFIED Brueckner, Helmut UNSPECIFIED UNSPECIFIED UNSPECIFIED
URN:	urn:nbn:de:hbz:38-197083
DOI:	10.1016/j.margeo.2017.03.005
Journal or Publication Title:	Mar. Geol.
Volume:	396
Page Range:	S. 186 - 205
Date:	2018
Publisher:	ELSEVIER SCIENCE BV
Place of Publication:	AMSTERDAM
ISSN:	1872-6151
Language:	English
Faculty:	Unspecified
Divisions:	Unspecified
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language PROGRADED BEACH DEPOSITS; SEA-LEVEL CHANGES; GRAIN-SIZE; GEOMORPHOLOGICAL EVIDENCE; TIBETAN PLATEAU; LATE-HOLOCENE; CLIMATE; TSUNAMI; COAST; SAND Multiple languages Geosciences, Multidisciplinary; Oceanography Multiple languages
Refereed:	Yes
URI:	http://kups.ub.uni-koeln.de/id/eprint/19708