Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography

As sea level rises, salt marshes become subtidal mudflats unless soil surface accretion occurs at rates fast enough to keep the marsh from being submerged (Brinson et al., 1995). The individual processes contributing to accretion are well known but vary geographically in their relative importance. W...

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Bibliographic Details
Main Authors: Linda K. Blum, Earl Davey
Format: Article
Language:English
Published: The Oceanography Society 2013-09-01
Series:Oceanography
Subjects:
Online Access:http://tos.org/oceanography/archive/26-3_blum.pdf
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author Linda K. Blum
Earl Davey
author_facet Linda K. Blum
Earl Davey
author_sort Linda K. Blum
collection DOAJ
description As sea level rises, salt marshes become subtidal mudflats unless soil surface accretion occurs at rates fast enough to keep the marsh from being submerged (Brinson et al., 1995). The individual processes contributing to accretion are well known but vary geographically in their relative importance. While the complicated interactions among accretion processes are poorly understood (Murray et al., 2008), production of roots and rhizomes is critical to maintenance of salt marsh soil structural integrity and marsh-surface elevation. Many long-term coastal research programs seek to understand how these interactions influence accretion to more accurately predict salt marsh response to sea level rise under widely differing rates of relative sea level rise, tide ranges, sediment supplies, nutrient inputs, coastal geomorphology, and climate.
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spelling doaj.art-e9bff8b043ef4152998657eb77c4536c2022-12-22T03:25:54ZengThe Oceanography SocietyOceanography1042-82752013-09-01263858710.5670/oceanog.2013.49Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided TomographyLinda K. BlumEarl DaveyAs sea level rises, salt marshes become subtidal mudflats unless soil surface accretion occurs at rates fast enough to keep the marsh from being submerged (Brinson et al., 1995). The individual processes contributing to accretion are well known but vary geographically in their relative importance. While the complicated interactions among accretion processes are poorly understood (Murray et al., 2008), production of roots and rhizomes is critical to maintenance of salt marsh soil structural integrity and marsh-surface elevation. Many long-term coastal research programs seek to understand how these interactions influence accretion to more accurately predict salt marsh response to sea level rise under widely differing rates of relative sea level rise, tide ranges, sediment supplies, nutrient inputs, coastal geomorphology, and climate.http://tos.org/oceanography/archive/26-3_blum.pdfLTERsea level risesalt marshsubtidal mud flat
spellingShingle Linda K. Blum
Earl Davey
Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
Oceanography
LTER
sea level rise
salt marsh
subtidal mud flat
title Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
title_full Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
title_fullStr Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
title_full_unstemmed Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
title_short Below the Salt Marsh Surface: Visualization of Plant Roots by Computer-Aided Tomography
title_sort below the salt marsh surface visualization of plant roots by computer aided tomography
topic LTER
sea level rise
salt marsh
subtidal mud flat
url http://tos.org/oceanography/archive/26-3_blum.pdf
work_keys_str_mv AT lindakblum belowthesaltmarshsurfacevisualizationofplantrootsbycomputeraidedtomography
AT earldavey belowthesaltmarshsurfacevisualizationofplantrootsbycomputeraidedtomography