Research Article| July 01, 1970 The Reef Flat and ‘Two-Meter Eustatic Terrace’ of Some Pacific Atolls NORMAN D NEWELL; NORMAN D NEWELL American Museum of Natural History, and Columbia University, New York, New York 10024 Search for other works by this author on: GSW Google Scholar ARTHUR L BLOOM ARTHUR L BLOOM Department of Geological Science, Cornell University, Ithaca, New York 14850 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1970) 81 (7): 1881–1894. https://doi.org/10.1130/0016-7606(1970)81[1881:TRFATE]2.0.CO;2 Article history received: 21 Aug 1969 rev-recd: 22 Feb 1970 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation NORMAN D NEWELL, ARTHUR L BLOOM; The Reef Flat and ‘Two-Meter Eustatic Terrace’ of Some Pacific Atolls. GSA Bulletin 1970;; 81 (7): 1881–1894. doi: https://doi.org/10.1130/0016-7606(1970)81[1881:TRFATE]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Characteristics of Indo-Pacific coral reefs long cited as evidence of a recent decline in sea level include: (1) the reef “flat” or pavement, (2) intertidal and supratidal flat erosion remnants of cemented coral rubble, and (3) erosion of the shores of reef islets.Our examination of 25 low islands and 8 high islands in the Caroline and Marshall Islands during the 1967 Scripps Institution of Oceanography Expedition CARMARSEL leads us to conclude that the reef flats in the western Pacific generally are not simply erosional platforms but represent an equilibrium surface between upward accretion by reef-building organisms and erosion at the mean level of low tides.Intertidal and supratidal coral rubble and calcareous sand accumulate above low-tide level during storms forming all of the visible land in the visited low islands. This rubble is currently being cemented and welded to the reef flats between tidal limits, and probably is also being cemented as beachrock and island conglomerate below the fluctuating water table of the cays.Topographically highest cemented carbonate rocks of the Caroline and Marshall Islands are uniformly less than 2 m above the adjacent reef flat, and entirely in the intertidal zone, hence, within the tidal range of present sea level.Flat horizontal surfaces of small extent occur on shore rocks, locally truncating inclined beds of beach rock. These surfaces roughly correspond to the upper limit of contemporary cementation somewhat modified by gravel scour. Comparison with rock platforms of a slightly elevated atoll of the Tuamotus, Raroia, indicates that the Marshall and Caroline Islands do not display expectable features of uplift or of subsiding sea level. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Read full abstract