Please cite this article in press as: Montefalcone, M., et al., Evaluating change in seagrass meadows: A time-framed comparison of Side Scan Sonar
maps. Aquat. Bot. (2011), doi:10.1016/j.aquabot.2011.05.009
ARTICLE IN PRESS
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AQBOT-2391; No. of Pages 9
Aquatic Botany xxx (2011) xxx–xxx
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Aquatic Botany
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Evaluating change in seagrass meadows: A time-framed comparison of Side Scan
Sonar maps
Monica Montefalcone
a,*
, Alessio Rovere
a,b
, Valeriano Parravicini
a,b
, Giancarlo Albertelli
a
,
Carla Morri
a
, Carlo Nike Bianchi
a
a
DipTeRis, Department for the study of the Territory and of its Resources, University of Genoa, Corso Europa 26, 16132 Genoa, Italy
b
SEAMap srl Environmental Consultancy, via Greto di Cornigliano 6R, 16152 Genoa, Italy
a r t i c l e i n f o
Article history:
Received 20 July 2010
Received in revised form 24 May 2011
Accepted 30 May 2011
Available online xxx
Keywords:
Seagrass
Mapping
Side Scan Sonar
Posidonia oceanica
Diachronic analysis
Mediterranean Sea
a b s t r a c t
Side Scan Sonar (SSS) is a common method for mapping seagrass meadows that allows to define
meadow extent and typology. Should sonogram interpretation be efficient, repeated mapping would
allow evaluation of spatial meadow dynamics through time. Here, maps of Posidonia oceanica (L.) Delile
meadows from western Liguria (NW Mediterranean Sea) produced in 1990, 1991 and 2006 through
SSS surveys, were processed with GIS (Geographical Information System) and compared by means of
diachronic analysis to establish concordances and discordances. While any difference between maps of
1990 and 2006 might provide information about change in seagrass cover with time, the availability
of maps taken at only one year of distance (1991 vs 1990) offered the unique opportunity to evalu-
ate the efficiency of SSS mapping, as the slow dynamics of P. oceanica makes significant change over
such a short time scale unrealistic in absence of any large-scale environmental catastrophe. Results
showed obvious differences in P. oceanica meadow distribution among the three periods in most of
the areas. The largest differences were found between the maps of 1990 and 1991. This discrepancy
was probably due to erroneous interpretation of small, fragmented shallow-water meadows on sono-
grams. Errors in sonogram interpretation combine with inefficient positioning in old cartographies
to blur the evaluation of change over large time scales (i.e. between 1990 and 2006). Extensive sea-
truthing based on a rigorous design is mandatory for efficient acoustic mapping of seagrass meadows.
© 2011 Elsevier B.V. All rights reserved.
1. Introduction
Marine cartography plays a key role for basic research, con-
servation and monitoring of marine ecosystems and for coastal
management purposes. The benthos is generally the target of
marine habitat mapping because of its greater structural com-
plexity, stability over time and space, and ability to record
environmental alterations as compared to open sea environments
(Bianchi et al., 2004).
Benthic cartography has a long tradition in the Mediterranean
Sea (Molinier and Picard, 1960; Meinesz, 1985) and assessment
of the status of coastal ecosystems has often involved seagrass
(Montefalcone et al., 2007a, 2007b, 2009; Boudouresque et al.,
2009; Waycott et al., 2009). Collection of reference state inventories
and baseline maps describing the current extent and condition of
seagrass meadows is priority in the light of the proper management
*
Corresponding author. Tel.: +39 010 3538584; fax: +39 010 3538140.
E-mail address: montefalcone@dipteris.unige.it (M. Montefalcone).
of such ecologically important ecosystems (Leriche et al., 2006). A
vast array of methods can be used for mapping seagrass. The choice
of which tool to use relies on the characteristics of the studied
area, the degree of accuracy required and the cost-effectiveness
in relation both to the time spent and the data acquisition scale
(Pasqualini et al., 2005 and reference therein).
The last two decades have seen rapid developments in the use of
digital data collected by remote sensing instruments (i.e. satellite
imagery, aerial photography, acoustic devices). Aerial photography,
in conjunction with image processing techniques, represents one of
the most efficient methods in terms of cost, rapidity and reliability
(Pasqualini et al., 1998, 1999), as it provides objective information
on entire meadows at a territorial spatial scale (Dekker et al., 2005).
While aerial and satellite imageries have been demonstrated to be
the best methods to draw the borders of shallow meadows, they
are not adequate for deeper meadows when water turbidity pre-
vents light penetration across the water column. Recent progress in
acoustic data acquisition and processing, together with improve-
ment in positional accuracy and computing power (McGonigle
et al., 2009), made the acoustic techniques, such as Side Scan Sonar
(hereafter SSS), echo sounders and multibeam, satisfactory alter-
0304-3770/$ – see front matter © 2011 Elsevier B.V. All rights reserved.
doi:10.1016/j.aquabot.2011.05.009