reference : Mangrove sedimentation and response to relative sea-level rise

JSON YAML text HTML Turtle N-Triples JSON Triples RDF+XML RDF+JSON Graphviz SVG
/reference/3bffd087-0af7-47d7-8a00-a21f0fc63569
Bibliographic fields
reftype Journal Article
Abstract Mangroves occur on upper intertidal shorelines in the tropics and subtropics. Complex hydrodynamic and salinity conditions, related primarily to elevation and hydroperiod, influence mangrove distributions; this review considers how these distributions change over time. Accumulation rates of allochthonous and autochthonous sediment, both inorganic and organic, vary between and within different settings. Abundant terrigenous sediment can form dynamic mudbanks, and tides redistribute sediment, contrasting with mangrove peat in sediment-starved carbonate settings. Sediments underlying mangroves sequester carbon but also contain paleoenvironmental records of adjustments to past sea-level changes. Radiometric dating indicates long-term sedimentation, whereas measurements made using surface elevation tables and marker horizons provide shorter perspectives, indicating shallow subsurface processes of root growth and substrate autocompaction. Many tropical deltas also experience deep subsidence, which augments relative sea-level rise. The persistence of mangroves implies an ability to cope with moderately high rates of relative sea-level rise. However, many human pressures threaten mangroves, resulting in a continuing decline in their extent throughout the tropics.*
Author Woodroffe, C. D.; Rogers, K.; McKee, K. L.; Lovelock, C. E.; Mendelssohn, I. A.; Saintilan, N.
DOI 10.1146/annurev-marine-122414-034025
Database Provider Annual Reviews
Date 2016
Issue 1
Journal Annual Review of Marine Science
Pages 243-266
Title Mangrove sedimentation and response to relative sea-level rise
Volume 8
Year 2016
Bibliographic identifiers
_record_number 22544
_uuid 3bffd087-0af7-47d7-8a00-a21f0fc63569