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29 novembre 2016
- handle: 10670/1.pgvftb
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Posidonia oceanea Velocity Quartz sand South Pacific Ocean Region South Pacific Region Islands--South Pacific Ocean South Seas South Pacific Oceanica Southwest Pacific Region South Sea Islands Colonisation VelocityCiter ce document
S. GOBERT et al., « Temporal evolution of sand corridors in a Posidonia oceanica seascape: a 15-years study », eJournals, ID : 10670/1.pgvftb
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Résumé
The spatial dynamic of Posidonia oceanica meadows is a process extending over centuries. This paper shows evidence of the natural dynamics of P. oceanica “shifting intermattes” or “sand corridors” (hereafter SCs): unvegetated patches within a dense meadow. We studied features and temporal evolution (2001-2015) of 5 SCs in the Calvi Bay (Corsica) at 15 m depth and followed the characteristics the P. oceanica meadow lining the edge of patches. All SCs show a similar topography. The eroded side is a vertical edge where roots, rhizomes and sediments are visible, when on the opposite colonized side, the sand is at the same level as the continuous meadow. The vertical edge reaches a maximum height of 160 cm and is eroded by orbital bottom currents with a maximum speed of 12 cm.s-1, the erosion speed ranging from 0.6 to 15 cm.y-1. SCs progress toward the coastline with a mean speed of 10 cm.y-1, the rate of colonization by P. oceanica shoots ranging from 1.5 to 21 cm.y-1. We calculated that the studied SCs would reach the coastline within 500 to 600 years. We finally discuss the implication of such dynamic in the framework of meadows’ colonization assessment and the seascape dynamic.