Sergio Dillenburg

Foredune vegetation patterns and alongshore environmental gradients: Moçambique Beach, Santa Catarina Island, Brazil

Publisher: Wiley

Date: 09-2008

DOI: 10.1002/ESP.1633

Discussion: “Evidence for a transgressive barrier within a regressive strandplain system: implications for complex response to environmental change” by Hein, et al. (2013), Sedimentology 60, 46

Publisher: Wiley

Date: 18-07-2014

DOI: 10.1111/SED.12132

Late-Holocene sea levels from vermetids and barnacles at Ponta do Papagaio, 27° 50′S latitude and a comparison with other sectors of southern Brazil

Publisher: Elsevier BV

Date: 06-2022

DOI: 10.1016/J.QUASCIREV.2022.107536

Holocene freshwater history of the Lower River Murray and its terminal lakes, Alexandrina and Albert, South Australia, and its relevance to contemporary environmental management

Publisher: Informa UK Limited

Date: 31-01-2022

DOI: 10.1080/08120099.2022.2019115

Coastal Barriers – An Introduction

Publisher: Springer Berlin Heidelberg

Date: 2009

DOI: 10.1007/978-3-540-44771-9_1

Reply to the discussion by Gell and Finlayson (2023)

Publisher: Informa UK Limited

Date: 26-02-2023

DOI: 10.1080/08120099.2023.2175908

Wave Energy as a Control on Dune Development on two Regressive Barriers in Southern Brazil

Publisher: Coastal Education and Research Foundation

Date: 03-03-2016

DOI: 10.2112/SI75-55.1

Geochronology and evolution of a complex barrier, Younghusband Peninsula, South Australia

Publisher: Elsevier BV

Date: 04-2020

DOI: 10.1016/J.GEOMORPH.2020.107044

Beach ridges, foredunes or transgressive dunefields? Definitions and an examination of the Torres to Tramandaí barrier system, Southern Brazil

Publisher: FapUNIFESP (SciELO)

Date: 09-2005

DOI: 10.1590/S0001-37652005000300010

Abstract: Many prograded barriers and some dunefields in theworld have been termed 'beach ridge' plains, but the actual genesis of the 'ridges' is often unknown. Use of the terms, berms, beach ridges and foredunes is also confusing in the literature because their definitions are highly variable and are commonly used interchangeably. Thus, the formation and definition of sand berms, beach ridges and foredunes is briefly reviewed. Beach ridges are re-defined as entirely wave formed deposits which are most commonly formed during high wave conditions and/or elevated water levels (e.g. storm surges). Foredunes are formed by aeolian sand deposition in vegetation on the backshore. Some dunefields in Brazil have been called beach ridge plains when they are, in fact, foredune plains, transgressive dunefields, or complex barriers (i.e. barriers comprising two types of dunes). The Holocene barrier extending from Torres to Tramandaí in southern Brazil has been regarded as a beach ridge plain. The landforms of this Holocene barrier comprise wide, relatively linear, widely spaced (400-600m), shore parallel ridges on the landward half, and more closely spaced (80-400m), lobate and crescentic, discrete ridges on the seaward half. Low, rolling dunefields, sand sheets, nebkha fields and deflation plains occur between the ridges. The barrier is re-interpreted as a prograded, transgressive dunefield barrier.

A large mid-Holocene estuary was not present in the lower River Murray, Australia

Publisher: Springer Science and Business Media LLC

Date: 08-06-2021

DOI: 10.1038/S41598-021-90025-9

Discovery Projects - Grant ID: DP220102926

Start Date: 05-2022

End Date: 04-2025

Amount: $378,000.00

Funder: Australian Research Council