GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard error; CDRILL; Core drilling; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; French Polynesia; Latitude of event; Longitude of event; TAH_VC8; TAH_VC9; δ13C, organic carbon  (1)
  • Alongshore sediment transport  (1)
Document type
Keywords
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Toomey, Michael R; Woodruff, Jonathan D; Donnelly, Jeffrey P; Ashton, Andrew D; Perron, J Taylor (2016): Seismic evidence of glacial-age river incision into the Tahaa barrier reef, French Polynesia. Marine Geology, 380, 284-289, https://doi.org/10.1016/j.margeo.2016.04.008
    Publication Date: 2023-02-08
    Description: Rivers have long been recognized for their ability to shape reef-bound volcanic islands. On the time-scale of glacial?interglacial sea-level cycles, fluvial incision of exposed barrier reef lagoons may compete with constructional coral growth to shape the coastal geomorphology of ocean islands. However, overprinting of Pleistocene landscapes by Holocene erosion or sedimentation has largely obscured the role lowstand river incision may have played in developing the deep lagoons typical of modern barrier reefs. Here we use high-resolution seismic imagery and core stratigraphy to examine how erosion and/or deposition by upland drainage networks has shaped coastal morphology on Tahaa, a barrier reef-bound island located along the Society Islands hotspot chain in French Polynesia. At Tahaa, we find that many channels, incised into the lagoon floor during Pleistocene sea-level lowstands, are located near the mouths of upstream terrestrial drainages. Steeper antecedent topography appears to have enhanced lowstand fluvial erosion along Tahaa's southwestern coast and maintained a deep pass. During highstands, upland drainages appear to contribute little sediment to refilling accommodation space in the lagoon. Rather, the flushing of fine carbonate sediment out of incised fluvial channels by storms and currents appears to have limited lagoonal infilling and further reinforced development of deep barrier reef lagoons during periods of highstand submersion.
    Keywords: Age, 14C AMS; Age, dated; Age, dated material; Age, dated standard error; CDRILL; Core drilling; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; French Polynesia; Latitude of event; Longitude of event; TAH_VC8; TAH_VC9; δ13C, organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Earth Surface 121 (2016): 664–683, doi:10.1002/2015JF003780.
    Description: River mouths, shoreline locations where fluvial and coastal sediments are partitioned via erosion, trapping, and redistribution, are responsible for the ultimate sedimentary architecture of deltas and, because of their dynamic nature, also pose great management and engineering challenges. To investigate the interaction between fluvial and littoral processes at wave-dominated river mouths, we modeled their morphologic evolution using the coupled hydrodynamic and morphodynamic model Delft3D-SWAN. Model experiments replicate alongshore migration of river mouths, river mouth spit development, and eventual spit breaching, suggesting that these are emergent phenomena that can develop even under constant fluvial and wave conditions. Furthermore, we find that sediment bypassing of a river mouth develops though feedbacks between waves and river mouth morphology, resulting in either continuous bypassing pathways or episodic bar bypassing pathways. Model results demonstrate that waves refracting into the river mouth bar create a zone of low alongshore sediment transport updrift of the river mouth, which reduces sediment bypassing. Sediment bypassing, in turn, controls the river mouth migration rate and the size of the river mouth spit. As a result, an intermediate amount of river discharge maximizes river mouth migration. The fraction of alongshore sediment bypassing can be predicted from the balance between the jet and the wave momentum flux. Quantitative comparisons show a match between our modeled predictions of river mouth bypassing and migration rates observed in natural settings.
    Description: NSF Grant Number: EAR-0952146
    Description: 2016-10-21
    Keywords: River mouth ; Bypassing ; Alongshore sediment transport ; Delft3D ; River mouth migration ; River mouth spit
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...