UNDERWATER SOUND RECORDING OF ANIMALS

ABSTRACT

Underwater sound recording of animals uses specialized techniques to obtain faithful copies of sounds produced by animals during their normal activities underwater. Techniques have to be unobtrusive as well as nondisturbing to avoid changing the animal behaviors. The first scientific recording of underwater sounds from a marine mammal at sea was by William E. Schevill and Barbara Lawrence in 1948. Although the equipment has changed considerably since then, the techniques, approaches to animals and environmental impediments have remained essentially the same. However, the frequency and dynamic ranges of underwater sounds can easily exceed terrestrial sounds, so the selection of suitable equipment is critical. The elements of a useful system for bioacoustic recording of marine animals include the hydrophone, impedance transformer/preamplifier, cable, signal amplifier, recorder and sound monitor. The important criteria for each of these is discussed, along with directional listening systems, and the need for calibrations to verify the performance of the entire underwater recording system. For each situation, the ideal system is the one with the best compromise of interactive components to record that particular sound spectrum.     

Effects of body size on selectivity for mating cues in different sensory modalities

We investigated the effects of body mass on the selectivity of female mating preferences in two different sensory channels (acoustic and chemical) using the field cricket, Gryllus integer. We found that body mass affected female selectivity for acoustic cues: larger females were more selective than smaller females for long‐distance calls of males. In contrast, body mass did not affect selectivity for chemical cues of males, which are assessed at close range. Nevertheless, we observed selectivity for these cues. Finally, selectivity for acoustic cues was not correlated with selectivity for chemical cues. These results suggest that energetic concerns may influence mating decisions made at a distance and that the effects of body mass on mating decisions are not necessarily shared across different sensory modalities. © 2011 The Linnean Society of London, Biological Journal of the Linnean Society, 2012, 105 , 160–168.     

The Development and Evolution of the Turtle Body Plan: Inferring Intrinsic Aspects of the Evolutionary Process from Experimental Embryology

The body plan of turtles is unique among tetrapods in the presenceof the shell. The structure of the carapace involves a uniquerelationship between the axial and the appendicular skeletons.A common developmental mechanism, an epithelial-mesenchymalinteraction, has been identified in the early stages of carapacedevelopment by means of basic histological and immunofluorescencetechniques. By analogy to other structures initiated by epithelial-mesenchymalinteractions, it is hypothesized that carapace development isdependent on this interaction in the body wall. Surgical perturbationswere designed to test the causal connection between the epithelial-mesenchymalinteraction in the body wall and the unusual placement of theribs in turtles. By comparison to data available on body wallformation in avian embryos, these experiments also shed lighton the segregation of somitic and lateral plate cell populationsand the embryonic origin of the scapula in turtles. This study specifically addresses the ontogeny of a unique tetrapodbody plan. The ontogenetic information can be used to make inferencesabout the phytogeny of this body plan and how it could haveevolved from the more typical primitive tetrapod. On a moregeneral level this studyexplores the potential role of commondevelopmental mechanisms in the generation of evolutionary novelties,and the developmental incongruities between homologous skeletalelements in different groups of tetrapods.     

Using DNA Barcodes to Identify Bird Species Involved in Birdstrikes

Abstract: We determined effectiveness of using mitochondrial DNA barcodes (cytochrome c oxidase subunit 1 [CO1]) to identify bird-aircraft collision (birdstrike) cases that lacked sufficient feather evidence for morphological diagnosis. From September through December 2006, 821 samples from birdstrike events occurring in the United States were submitted for DNA analysis. We successfully amplified a CO1 DNA barcode product from 554 (67.5%) of the samples; 267 (32.5%) did not contain viable DNA and depended on morphological methods (microscopy) for Order or Family level identification. We deemed 19 cases inconclusive either because the DNA barcode recovered from the sample did not meet our 98% match criteria when compared to the Barcode of Life Database (BoLD) or because the DNA barcode matched to a set of ≥ 2 closely related species with overlapping barcodes, preventing complete species identification. Age of the sample (≤6 months) did not affect DNA viability, but initial condition of the sample and the collection method was critical to DNA identification success. The DNA barcoding approach has great potential in aiding in identification of birds (and wildlife) for airfield management practices, particularly in regions of the world that lack the vast research collections and individual expertise for morphologic identifications.     

Sphaerospora ictaluri N. Sp. (Myxosporea: Sphaerosphoridae) Observed in the Kidney of Channel Catfish, Ictalurus punctatus Rafinesque

Sphaerospores were found in the kidneys of alevin channel catfish (Ictalurus punctatus) from a farm in Central California. MulticelluUr developmental stages, similar to C-blood protozoans described for Sphaerospora spp. from cyprinid fishes, were observed in circulating blood and numerous tissues. Upon a 2nd examination of the same population offish 10 days later, sporogonic stages were seen developing into mature Sphaerospores in the lumina of the kidney tubules. Sporogeoesis was asynchronous with simple unicellular stages adjacent to more complex forms with developing polar capsules and valves. Only one elliptical spore (5.6 μm in width, 6.5 μm in thickness by 5.8 μm in length) developed within the surrounding pscudoplasmodium. Thin valves surrounded two sporoplasm cells and two subspherical polar capsules (1.7 × 1.9 μm) which contained a polar filament with four to five turns. The blood stages of the Sphaerospora sp. described here are similar to the trophozoites seen in channel catfish with proliferativc gill disease (PGD). Early stages of PGD also observed in the same population of channel catfish containing developmental and sporogonic stages of this newly recognized Sphaerospora sp. may suggest a causal relationship between this new myxosporean and the gill disease.     

Y chromosome microsatellite markers identified from the tammar wallaby (Macropus eugenii) and their amplification in three other macropod species

Microsatellites were identified from three fully sequenced Y chromosome‐specific bacterial artificial chromosome clones from the tammar wallaby, Macropus eugenii. Ten microsatellites were genotyped in male tammar wallabies. Four loci were polymorphic with between two and six alleles per locus. Eleven different haplotypes were identified from 22 male tammar wallabies. No amplifications were obtained from female samples. Each microsatellite was also shown to amplify reliably in at least one other macropod species. These markers may therefore prove useful as some of the first male‐specific genetic markers for marsupials, with potential application to studies of male‐biased dispersal and mating systems.     

How strong is the current carbon sequestration of an Atlantic blanket bog?

Although northern peatlands cover only 3% of the land surface, their thick peat deposits contain an estimated one‐third of the world's soil organic carbon (SOC). Under a changing climate the potential of peatlands to continue sequestering carbon is unknown. This paper presents an analysis of 6 years of total carbon balance of an almost intact Atlantic blanket bog in Glencar, County Kerry, Ireland. The three components of the measured carbon balance were: the land‐atmosphere fluxes of carbon dioxide (CO₂) and methane (CH₄) and the flux of dissolved organic carbon (DOC) exported in a stream draining the peatland. The 6 years C balance was computed from 6 years (2003–2008) of measurements of meteorological and eddy‐covariance CO₂ fluxes, periodic chamber measurements of CH₄ fluxes over 3.5 years, and 2 years of continuous DOC flux measurements. Over the 6 years, the mean annual carbon was ?29.7±30.6 (±1 SD) g C m^?2 yr^?1 with its components as follows: carbon in CO₂ was a sink of ?47.8±30.0 g C m^?2 yr^?1; carbon in CH₄ was a source of 4.1±0.5 g C m^?2 yr^?1 and the carbon exported as stream DOC was a source of 14.0±1.6 g C m^?2 yr^?1. For 2 out of the 6 years, the site was a source of carbon with the sum of CH₄ and DOC flux exceeding the carbon sequestered as CO₂. The average C balance for the 6 years corresponds to an average annual growth rate of the peatland surface of 1.3 mm yr^?1.