Elsevier

Remote Sensing of Environment

Volume 112, Issue 11, 15 November 2008, Pages 4159-4165
Remote Sensing of Environment

Using bathymetric lidar to define nearshore benthic habitat complexity: Implications for management of reef fish assemblages in Hawaii

https://doi.org/10.1016/j.rse.2008.01.025Get rights and content

Abstract

Habitat complexity plays a major role in determining the distribution and structure of fish assemblages in the aquatic environment. These locations are critical for ecosystem function and have significant implications for conservation and management. In this study, we evaluated the utility of remotely sensed lidar (light detection and ranging) data for deriving substrate rugosity (a measure of habitat complexity) on a coral reef in Hawaii. We also assessed the potential application of lidar data for examining the relationship between habitat complexity and Hawaiian reef fish assemblage characteristics. Lidar-derived rugosity (4 m grid size) was found to be highly correlated with in-situ rugosity and was concluded to be a viable method for measuring rugosity in analogous coral reef environments. We established that lidar-derived rugosity was a good predictor of fish biomass and demonstrated a strong relationship with several fish assemblage metrics in hard bottom habitat at multiple spatial resolutions. This research demonstrates (i) the efficacy of lidar data to provide substrate rugosity measures at scales commensurate with the resources and their environment (ii) the applicability of lidar-derived rugosity for examining fish–habitat relationships on a coral reef in Hawaii and (iii) the potential of lidar to provide information about the seascape structure that can ultimately be used to prioritize areas for conservation and management.

Introduction

Habitat complexity in the coastal environment plays an important role in structuring nearshore fish assemblages. The relationship between habitat complexity and measures of community structure was first observed in the terrestrial realm (August, 1983, MacArthur and MacArthur, 1961, Murdoch et al., 1972, Rosenzweig and Winakur, 1969). A similar relationship between habitat complexity and fish assemblage characteristics has been well documented in both freshwater (Gorman & Karr, 1978) and marine ecosystems (Caley and St John, 1996, Friedlander and Parrish, 1998, Gratwicke and Speight, 2005, Luckhurst and Luckhurst, 1978, Risk, 1972, Roberts and Ormond, 1987).

Structural complexity, a major component of habitat complexity, can be defined as the architecture of the physical environment (McCoy and Bell, 1991, Sebens, 1991). Structurally complex habitats offer more potential niches and increase survivorship by providing fish additional refuge from predation (Almany, 2004, Beukers and Jones, 1998, Hixon and Beets, 1989). Accordingly, areas of high structural complexity harbor high species richness (Gratwicke & Speight, 2005), species diversity (Almany, 2004) and fish biomass (Friedlander & Parrish, 1998).

There are a number of habitat complexity variables that can be measured in-situ (reviewed in McCormick, 1994), and rugosity is the most commonly used in-situ measure. For the purposes of this study, rugosity, or vertical relief, was used to represent a measure of structural complexity. The chain transect method measures in-situ rugosity by obtaining the ratio of the length of a chain laid across the bottom profile along a transect line to the linear distance of the transect line (Friedlander and Parrish, 1998, Luckhurst and Luckhurst, 1978, Risk, 1972). A limitation of the traditional chain transect method is the restriction of the structural complexity measurements to relatively fine spatial scales. Additionally, field measurements are time-consuming, can have high inter-observer variability, and are difficult to obtain over a broad geographic area.

Considering the documented importance of the relationship between rugosity and fish assemblage structure, it is critical to develop faster methods of determining rugosity in the marine environment at broader geographic extents. The current expansion and wide application of remote sensing technology on coral reef ecosystems were recently reviewed (Mumby et al., 2004). Lidar (Light detection and ranging) is an active remote sensor that allows for spatial analysis of structurally complex habitats (Lefsky et al., 2002). Lidar has recently been applied to map coral reef structure (Storlazzi et al., 2003), and to measure reef rugosity (Brock et al., 2004, Brock et al., 2006). Lidar can provide measurements that may be scaled to allow for extraction of information at spatial extents that are more appropriate for coral reef ecosystems and related management actions. Applying remote sensing techniques that can rapidly identify structurally complex habitat may greatly assist resource managers in locating areas that are important to protect and sustain nearshore fish populations.

The goals of this study were (1) to determine whether lidar technology can provide effective rugosity measures on a coral reef in Hawaii and (2) to examine the relationship between reef fish assemblage characteristics and lidar-derived rugosity.

Section snippets

Study area

The study area is located in the Hanauma Bay Marine Life Conservation District (MLCD) on the south shore of the island of Oahu, in the Hawaiian Archipelago (Fig. 1). Hanauma Bay MLCD was designated as the first “no-take” marine protected area (MPA) in Hawaii in 1967 and encompasses approximately 41 ha. This area receives over one million visitors per year and is the most visited MPA in the world (Friedlander et al., in review). The bay was formed by the collapse of two volcanic craters, with

Lidar data processing

Digital elevation models (DEMs) are commonly produced from lidar data in order to calculate habitat structural complexity (Knudby et al., 2007). DEMs of Hanauma Bay were created at four grid cell sizes (4, 10, 15 and 25 m grids) from the lidar data using GS+ (Gamma Design Software). Conditional simulation was used to create the digital elevation models. Conditional simulation is a geostatistical method that assumes spatial autocorrelation of the data and creates random realizations that possess

Benthic terrain analysis

Bathymetric grids were created at four spatial resolutions from the lidar data (Fig. 4) and rugosity values were derived from the rugosity index maps for each grid size (Fig. 5). The result of the Spearman rank correlations demonstrated that the lidar-derived rugosity at the 4 m grid size had a significant positive association (r = 0.61, P < 0.01) with the in-situ rugosity, but the 10, 15, and 25 m grid sizes did not show statistically significant associations (Table 2).

Relationship between in-situ rugosity and fish assemblages

In-situ rugosity

The utility of lidar to provide effective rugosity measures on a coral reef in Hawaii

Lidar-derived rugosity (4 m grid size) was found to be highly correlated with in-situ rugosity and represents a viable method for measuring rugosity in analogous coral reef environments. The lidar-derived rugosity in our study represented an area-based measurement, and the chain method used in-situ was a linear measurement of habitat complexity. Despite the fact that these two methods used in our study were measuring habitat complexity using different approaches, the results demonstrated a

Conclusions

The first goal of this study was to determine whether lidar technology could provide effective rugosity measures on a coral reef in Hawaii. Lidar was found to provide valuable rugosity measures at our study site and our findings extend prior work in Florida patch reefs (Brock et al., 2004, Kuffner et al., 2007) to a contiguous coral reef environment in Hawaii. The second goal of this study was to examine the relationship between reef fish assemblage characteristics and lidar-derived rugosity.

Acknowledgements

We would like to thank Athline Clark, Paul Jokiel, Eric Brown and Alan Hong for their support during this project. Simon Pittman, Steve Rohmann, Ariel C. Rivera-Vicente, Matthew Barbee and three anonymous reviewers provided valuable comments on this manuscript. The U.S. Army Corps of Engineers contributed the SHOALS lidar data used for this study. This research was funded by NOAA's Coral Reef Conservation Program and National Centers for Coastal Ocean Science-Center for Coastal Monitoring and

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