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  4. Relative sea-level changes and reef development in the northern Coral Triangle during the late Quaternary
 
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Relative sea-level changes and reef development in the northern Coral Triangle during the late Quaternary

Journal
Geomorphology
Journal Volume
483
Start Page
109796
ISSN
0169-555X
Date Issued
2025-08
Author(s)
Maxwell, Kathrine
Rovere, Alessio
Westphal, Hildegard
Garas, Kevin
Guinto, Mirasol
Chauveau, Denovan
Hu, Hsun-Ming
Shen, Chuan-Chou  
DOI
10.1016/j.geomorph.2025.109796
URI
https://www.scopus.com/pages/publications/105004880148
https://scholars.lib.ntu.edu.tw/handle/123456789/734814
Abstract
The Philippines, situated at the apex of the Coral Triangle, is fringed by both modern and fossil coral reefs that preserve valuable records of Quaternary relative sea-level changes and tectonic deformation. This study presents a new interpretation of the formation of the Late Pleistocene coral reef terraces at Cape Bolinao in western Luzon, offering insights into sea-level history, reef development, and tectonic uplift within the northern Coral Triangle. Integrating high-resolution morphological analysis, new geochronological data, and reef stratigraphic numerical models, we delineate nine distinct reef terraces. The lowest terrace (∼4 m above mean sea level) dates to the mid-Holocene, while reef simulations replicating present-day terrace morphology constrain the highest terrace (∼155 m amsl) to Marine Isotope Stage (MIS) 5e, indicating a long-term uplift rate of 1.17 ± 0.03 mm/yr for Cape Bolinao. We propose a morpho-chronologic framework wherein a Late Pleistocene table reef developed on a gently sloping substrate and was progressively uplifted, leading to successive fringing reef terraces. This high uplift, coupled with observed tilting and deformation patterns, provides compelling evidence that subduction of the Scarborough Seamount Chain beneath Luzon Island exerts a primary control on localized forearc deformation along the Manila Subduction Zone. This work offers a key dataset for understanding Quaternary CRT development in the northern Coral Triangle and sheds light on how subduction-related processes have shaped the region's sea-level and coral reef records.
Subjects
Coral reef terraces
Coral Triangle
Late Quaternary
Relative sea-level change
SDGs

[SDGs]SDG13

Publisher
Elsevier BV
Type
journal article

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