On the generation and degradation of emerged coral reef terrace sequences: First cosmogenic 36Cl analysis at Cape Laundi, Sumba Island (Indonesia). (1st October 2021)

• Record Type: Journal Article
• Authors: Chauveau, Denovan; Authemayou, Christine; Pedoja, Kevin; Molliex, Stéphane; Husson, Laurent; Scholz, Denis; Godard, Vincent; Pastier, Anne-Morwenn; de Gelder, Gino; Cahyarini, Sri Yudawati; Elliot, Mary; Weber, Michael; Benedetti, Lucilla; Jaud, Marion; Boissier, Audrey; Agusta, Vera Christanti; Aribowo, Sonny; Budd, Ann F.; Natawidjaja, Danny Hilman
• Is Part Of: Quaternary science reviews. Volume 269(2021)
• Publication Date: 2021-10-01
• Subjects: Quaternary -- Coral reef terrace -- 36Cl cosmogenic isotope -- Denudation rate -- U–Th series -- Coastal erosion -- MIS 5 -- Southeastern asia; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2021.107144
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: The emerged coral reef terrace sequence at Cape Laundi, on the north coast of Sumba Island (Indonesia), with at least 18 successive strandlines, remains poorly dated in spite of numerous previous data. The age discrepancies within these coral reef terraces (CRTs) were previously explained by their polycyclic nature, triggered by marine erosion and reoccupation of old coral colonies by new ones. This study aims at highlighting these processes, as well as the continental denudation that participates in the partial stripping of the thin superficial coral reef layer overlying the pre-existing surface, exhuming older coral colonies. For this purpose, we use a combined analysis of 36 Cl cosmogenic concentrations, new 230 Th/U ages, and previous dating in order to quantify denudation rates affecting the sequence and to highlight the role of marine erosion in reworking the lowest CRT surface. Our results demonstrate that 1) the lowermost CRT is composite, i.e., formed by different reefal limestone units constructed and eroded during successive highstands of the last interglacial, 2) following the last deglaciation, this CRT has been subjected again to coastal erosion and reoccupation during the Mid Holocene highstand, 3) its distal edge is affected by the current marine erosion and shows denudation rates higher by one to two orders of magnitude (from 279 ± 0.4 to 581 ± 0.4 mm ka −1 ) than the continental denudation values of higher CRTs (14.7 ± 8.3 mm ka −1 on average), 4) at the scale of a single CRT surface, variations in continental denudation rates are caused by epikarstification roughness, and 5) the distal edges have the highest continental denudation rate due to diffusion and regressive erosion produced by the runoff occurring along the steep downward cliff. Highlights: Coral reef terraces at Cape Laundi (Sumba Island) have a polycyclic nature. An analysis of 36 Cl cosmogenic concentrations on terraces to quantify continental denudation and marine erosion rates. Marine erosion and continental denudation explained the age diachronism on a single terrace. The lower terraces experienced alternating construction and erosion phases during highstands of the last interglacial. Marine erosion rates are much higher by one to two orders of magnitude than the continental denudation rates.