Assessing marine ecosystem acoustic diversity across ocean basins
Introduction
Acoustic recordings provide a relatively low-cost method of collecting data on sound sources in the environment. Passive acoustic monitoring can provide a continuous record of acoustic signals of interest, and the scope of these monitoring systems ranges from short duration, single point recordings to vast sensory networks that span the globe (Blumstein et al., 2011, Fox et al., 1978–2012). Historically, long-term continuous acoustic monitoring was limited to low-frequency/bandwidth sensors due to constraints in power consumption, data storage, or installation costs. In recent years, costs related to power consumption and data storage space have been drastically reduced. This has resulted in a dramatic increase in the number of long-term continuous acoustic recordings being collected at higher sample rates. Acoustic monitoring has been utilized in a wide range of applications, ranging from long-term low frequency units that have been used to measure seismic activity (Fox et al., 2001) to higher frequency regional data collected using both autonomous and cabled systems (Wiggins and Hildebrand, 2007, Zaugg et al., 2010).
A major challenge that comes with these long-term datasets is the management of the vast quantities of data that are collected. Data can come from continuous long-term recordings (months or years in duration) from multiple sensors, resulting in a veritable flood of information (Fox et al., 1978–2012, Lammers et al., 2008). Manual inspection, based on visual or aural inspection, of these large acoustic datasets quickly becomes impractical (Swiston and Mennill, 2009, Urazghildiiev and Clark, 2007). Over the past two decades, multiple approaches toward automated and semi-automated processing of terrestrial and aquatic recordings have been developed and range from assessment of ambient background noise to specific detailed analysis of acoustic behavior of individual species (Blumstein et al., 2011, Mellinger and Clark, 1997, Mellinger et al., 2007, Urazghildiiev and Clark, 2007).
Quantifying biological diversity is a vital aspect of conservation biology to allow for ecosystem monitoring to inform conservation and management efforts (Gotelli and Colwell, 2001, Pimm and Lawton, 1998). An emerging area of research is the use of statistical analyses of data collected with remote sensors to rapidly assess biodiversity or ecosystem health (Sueur et al., 2008, Turner et al., 2003). Acoustic remote sensing data is well suited for detection and as an indirect measure of the biodiversity of sound producing organisms (Riede, 1993, Sueur et al., 2008) and of human disturbance associated with anthropogenic noise (Barber et al., 2010).
Automated acoustic indices have been used to indirectly assess acoustic biodiversity including the quantification of temporal and spectral acoustic entropy (Ht and Hf) (Sueur et al., 2008), temporal and spectral dissimilarity indices (Dt, Df) (Gasc et al., 2013, Sueur et al., 2008), and metrics to capture diversity, evenness, richness, and dominance (Villanueva-Rivera et al., 2011). These approaches have been utilized to investigate acoustic diversity in two terrestrial habitats, including woodlands and tropical forests (Depraetere et al., 2012, Sueur et al., 2008). Studies using realistic field data indicate that background noise can unduly influence entropy measurements, leading to necessary refinement in the analysis procedures including pre-filtering for background noise and calculating the median values of overall signal amplitude (M) (Depraetere et al., 2012).
These statistical acoustic indices have not yet been applied to marine acoustic recordings. Previous underwater studies have used a variety of methods to characterize annual variation in long-term marine acoustic recordings (Hatch et al., 2008, Lammers et al., 2008, Miksis-Olds et al., 2012, Nieukirk et al., 2012). In general, marine systems are often dominated by abiotic sound sources (weather, seismic events) (Wenz, 1962) and increasing levels of human generated noise (Slabbekoorn et al., 2010). Reduced levels of transmission loss of acoustic energy in the marine environment when compared to air, result in greater ranges of acoustic propagation. This results in the ability to detect acoustic signals at greater distances, increasing the effective range of distant abiotic and anthropogenic sources of acoustic energy competing with the acoustic energy contribution from local biotic species. This exploratory study applies the acoustic entropy indices developed for terrestrial recordings (Sueur et al., 2008) to low frequency marine recordings from three oceans to assess the effectiveness of this method in quantifying differences in acoustic biodiversity between sites, between seasons, and in differing background noise conditions in the marine environment.
Section snippets
Acoustic dataset
Acoustic data from the Preparatory Commission for the Comprehensive Nuclear Test Ban Treaty International Monitoring System (CTBT IMS) in the South Atlantic (Ascension Island, H10, 8.0°S, 14.4°W), Indian (Diego Garcia, H08, 7.3°S, 72.4°E) and North Pacific (Wake Island, H11, 19.3°N, 166.6°E) ocean basins were obtained from the AFTAC/US NDC (Air Force Tactical Applications Center/ US National Data Center) (Fig. 1). Each CTBT IMS location consists of a cabled 3-hydrophone array with a frequency
Results
Acoustic recordings from one hydrophone in each of the three ocean basins contained numerous acoustic signals (Fig. 3). Natural seismic activity, including earthquakes and volcanic activity, was detected at all three sites and was present almost 100% of the time in each ocean (Fig. 5). Acoustic calls from three species of baleen whales were detected among the three sites. These include fin whales (Balaenoptera physalus), blue whales (Balaenoptera musculus sp.) and sei whales (Balaenoptera
Discussion
It is challenging to rapidly assess biodiversity over relevant spatio-temporal scales, given the variable composition of communities regionally and seasonally in a particular location. In the marine environment, where direct visual observation is often not feasible, remote sensing will likely provide the most useful way forward. Acoustic monitoring, with the potential for relatively low-cost, long-term monitoring of sites, is already providing these types of data on a global scale in the marine
Acknowledgments
The authors would like to acknowledge the editors for organizing this special issue and providing us an opportunity to explore acoustic diversity in marine settings. We would like to give special thanks to J. Sueur and D. Cusano for the advice and constructive comments on the early drafts of this paper. Thanks are extended to James Neely (AFTAC), Richard Baumstark (AFTAC), Mark Prior (CTBTO), Andrew Forbes (CTBTO), and Georgios Haralabus (CTBTO) for their assistance in data transfer and
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