Thecosome pteropods (Mollusca, Gastropoda) are an ecologically important, diverse, and ubiquitous group of holoplanktonic animals that are the focus of intense research interest due to their external aragonite shell and vulnerability to ocean acidification. Characterizing the response of these animals to low pH and other environmental stressors has been hampered by continued uncertainty in their taxonomic identification. An example of this confusion in species assignment is found in the genus Diacavolinia. All members of this genus were originally indentified as a single species, Cavolinia longirostris, but over the past fifty years the taxonomy has been revisited multiple times; currently the genus comprises 22 different species. This study examines five species of Diacavolinia, including four sampled in the Northeast Atlantic (78 individuals) and one from the Eastern tropical North Pacific (15 individuals). Diacavolina were identified to species based on morphological characteristics according to the current taxonomy, photographed, and then used to determine the sequence of the “DNA barcoding” region of the cytochrome c oxidase subunit I (COI). Specimens from the Atlantic, despite distinct differences in shell morphology, showed polyphyly and a genetic divergence of <3% (K2P distance) whereas the Pacific and Atlantic samples were more distant (~19%). Comparisons of Diacavolinia spp. with other Cavolinia spp. reveal larger distances (~24%). These results indicate that specimens from the Atlantic comprise a single monophyletic species and suggest possible species-level divergence between Atlantic and Pacific populations. The findings support the maintenance of Diacavolinia as a separate genus, yet emphasize the inadequacy of our current taxonomic understanding of pteropods. They highlight the need for accurate species identifications to support estimates of biodiversity, range extent and natural exposure of these planktonic calcifiers to environmental variability; furthermore, the apparent variation of the pteropods shell may have implications for our understanding of the species’ sensitivity to ocean acidification.
Citation: Maas AE, Blanco-Bercial L, Lawson GL (2013) Reexamination of the Species Assignment of Diacavolinia Pteropods Using DNA Barcoding. PLoS ONE 8(1): e53889. doi:10.1371/journal.pone.0053889
Editor: Sharyn Jane Goldstien, University of Canterbury, New Zealand
Received: August 2, 2012; Accepted: December 4, 2012; Published: January 15, 2013
Copyright: © 2013 Maas et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This material is based upon work supported by the National Science Foundation under Grant Number OCE-0928801. AEM was funded through the WHOI Postdoctoral Scholarship. Support to LBB was provided by the College of Liberal Arts & Sciences, University of Connecticut; and by the Census of Marine Life/Alfred P. Sloan Foundation. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Thecosome pteropods (Mollusca, Gastropoda) are a group of holoplanktonic animals that have been the focus of recent research because of their susceptibility to ocean acidification . Bearing thin aragonite shells, the calcification of these animals has been shown to be reduced when they are exposed to the projected changes in surface water pH and saturation state of the future ocean , , . Studies of metabolism, however, reveal a complex sensitivity to pH dependent upon natural exposure and synergistic stressors , , . Understanding the response of these animals to ocean acidification, and understanding the broader ecosystem impacts of their sensitivity, has been slowed by a serious lack of information about the ecology, physiology and ecosystem function of pteropods. Although the ecological importance of pteropods is not clearly established, it is known that pteropods can become a numerically dominant member of the zooplankton community in temperate and polar seas  and it has been hypothesized that the species Limacina inflata is the most abundant gastropod in the world . Growing research suggests that pteropods can be significant consumers of primary production , , , substantially contribute to carbon flux , , , , and serve as a key food item for a number of species including other zooplankton, fish, seabirds and whales , , , , , , .
Our expanding understanding of the importance of pteropods in food webs and biogeochemical cycling is complicated by a lack of clarity in the taxonomic literature for this group. As the ocean environment changes as a result of the complex interaction between rising temperature, changing O2 availability, shoaling of the saturation horizon for calcium carbonate compounds, as well as differences in water pH, it becomes more important to differentiate between distinct species in order to understand functional variability and resilience at population levels. Furthermore, in conjunction with generation time, high levels of genetic variability within a population may differentiate between species or populations that survive and those which are lost as the environment changes due to anthropogenic forcing , , . The distribution and diversity of pteropod species, however, remains in question.
Pteropods, consisting of the two orders Thecosomata (shelled) and Gymnosomata (naked), have had a tumultuous systematic history starting in the 1800’s . Originally grouped in the class of Pteropoda, only recently have they been regrouped with opisthobranchs and reunited as monophyletic sister taxa under the Gastropod class of Opisthobranchia using modern molecular techniques , . The early taxonomic work on thecosomes was dependent upon net tow samples of formalin-preserved, frequently unbuffered specimens, and the recent traditional classification is marked by a high degree of “splitting” into species, subspecies, and formae . Preserved thecosomes are frequently difficult to identify, as many of the delicate external morphological features diagnostic of some families, such as the gelatinous pseudoconch and the long external mantle appendages, are never seen in a natural conformation in net-captured animals . Consequently, taxonomists have traditionally used the less delicate aragonitic shell to classify and identify organisms, despite the tendency of this structure to dissolve in acidic preservation techniques. This classical shell-based morphological taxonomy described a group which consists of a number of cosmopolitan or bipolar species found in multiple ocean basins, with variations in shell shape, size and color that transition over latitudinal or ocean basin scales and that have often been designated as sub-specific formae , . Over time it has become clear that reliance solely upon shell morphology is an inadequate way of describing inter- and intra-species level variation in pteropods, and a number of designations have been reassessed. For example, populations of Limacina helicina, one of the most abundant pteropods and the dominant thecosome in polar regions, were originally believed to be the same species in the Arctic and Antarctic, but have recently been shown through genetic, behavioral, and physiological factors to be separate at a species level . Furthermore, work spanning the various pteropod families indicates that although some circumglobal distributions and forma gradations are supported by genetic evidence, others are not, suggesting the need for closer examinations of the taxonomic classification of several pteropod genera .
The genus Diacavolinia (Order Thecosomata, Suborder Euthecosomata, Family Cavoliniidae, Subfamily Cavoliniinae) , , is one of the most heavily radiated groups, and is the most recently established taxonomic classification within the pteropods. Of the shelled pteropods, the Cavoliniinae are thought to be the most derived, having developed gills and the most complex mantle structures of the thecosomes, theoretically to provide greater surface area and stability in the planktonic environment , . The Diacavolinia are a common and sometimes very abundant genus of subtropical thecosomes which were originally classified as one species, Cavolinia longirostris . As a result of the findings of Tesch, during the Dana expeditions, this species was later re-classified as having three formae: longirostris, strangulata, and angulata/angulosa , , . From these expeditions, which sampled extensively in Indo-Malayan waters and more sparsely from 20° N –40° S in the Atlantic Ocean, the first biogeography of this group was established with strangulata and angulata/angulosa absent from the Atlantic, and the Atlantic forma, longirostris, occasionally found in Indo-Pacific samples. The variability in shell morphology within these formae is mentioned by Tesch who described the Cavolinia longirostris angulata forma of the Pacific voyage as having a characteristic bifid rostrum, although noting that the rostrum was sometimes completely absent from similarly-sized specimens . In Atlantic specimens Tesch notes that there was quite a range in animal size and that in smaller animals the rostrum, as well as the side-processes (spines), were significantly less developed .
In the early 1970’s van der Spoel re-examined the species Cavolinia longirostris, increased the number of forma to six, adding limbata, flexipes and mcgowani, and suggested that there were more clear basin level differences in their distribution , , . The formae longirostris and limbata were assigned cosmopolitan distribution, strangulata was documented as inhabiting the Atlantic and Pacific basins, angulosa was found in the Indo-Pacific, flexipes in the Red Sea, and mcgowani exclusively in the Pacific Ocean . In contrast to McGowan  who felt that variations in shell type were dependent upon variation in environmental conditions and a high degree of phenotypic plasticity, van der Spoel cited the consistency of distributional patterns and an unclear mechanism for the genesis of the distinct shell angles and characteristics to justify the naming of multiple formae. In time the species Cavolinia longirostris was raised to genus level, and renamed as Diacavolinia longirostris , based on the fact that individuals of the species lose their juvenile protoconch-I and –II in a different way from all other members of the Cavoliniinae subfamily. Finally in 1993, after an extensive review of museum specimens, van der Spoel and colleagues reorganized the genus and elevated the formae to species, after which it contained 22 species, one of which retained 2 formae. He argued that separate species were necessary based on the fact that there were no geographic patterns in their variation and no zones of transition; although he noted that sympatry of these different species was very common, he stated that individuals could accurately be identified in mixed samples.
These arguments, particularly the extreme frequency of sympatry, raise the question of what form of niche partitioning or mechanism of evolutionary differentiation could lead to such a variety of closely-related species coexisting in the plankton. Van der Spoel and his colleagues suggested that an improved separation of the male and female parts and the presence of a closed gonoduct may have produced rapid radiation of the genus . Furthermore, since this group undergoes rapid growth of the adult teloconch shell followed only by minor additions of shell along the aperture and spines, van der Spoel et al.  asserted that co-occurrence of different shell sizes and shapes could not be a product of ontogenetic variation since the shapes cannot be explained through linear growth. Disentangling the identification of these species and the importance of ontogeny is made complicated, however, by the facts that the key established by van der Spoel et al.  is based exclusively on slight variations in shell shape and can only be used on adult animals. If valid, the apparent high degree of diversity in this genus could be associated with interesting physiological and ecological differences between co-occurring and recently separated species, meriting further investigation. Overall, due to the complexity of the species assignments of this group, Diacavolinia may benefit from reanalysis with the addition of modern molecular taxonomic techniques.
One of the approaches to address such questions is the use of DNA barcoding . This technique enables the recognition and discrimination of an individual’s species based on a conserved short DNA sequence present in all genomes; the most commonly accepted for metazoans being a fragment from the gene for the mitochondrial cytochrome c oxidase subunit I . DNA barcoding has been applied to a wide range of marine metazoans , including pteropods , . Although subject to confusion and controversy about its use as a taxonomic instrument per se , , , this technique has proven to be a powerful tool for addressing and resolving systematic problems, when combined with traditional morphological, ecological, and physiological methods . DNA barcoding is especially useful when morphological discrimination is difficult or impossible (e.g., early life stages, subtle or lacking diagnostic characters, cryptic species).
The objective of this study is to reexamine the species assignment of Diacavolinia pteropods using DNA barcoding. Individuals sampled in the Atlantic and Pacific Oceans were identified to species following the morphology-based key of van der Spoel et al. , and then genetically analyzed at the cytochrome c oxidase subunit I barcoding region. Additional insight was also gained by comparing individuals of the Diacavolinia genus to species from the closely-related Cavolinia genus. The resulting findings about biodiversity and population level variability were considered in light of their implications for pteropod response to environmental stressors, such as ocean acidification.
Specimen Collection, Preservation, and Morphological Analysis
Individuals collected for morphological and later genetic analysis were sampled during cruise OC 473 on the RV Oceanus (August 2011) in the Northwest Atlantic. Individuals from the eastern tropical North Pacific, obtained aboard the RV Seward Johnson (October and November 2007) were also analyzed. Samples from the Northwest Atlantic were captured using either a 1 m diameter, 150 µm mesh Reeve net towed through the upper 100 m at night or vertically stratified casts of a 1 m2 Multiple Opening/Closing net and Environmental Sensing System (MOCNESS) equipped with 150 µm mesh nets . Pacific samples were collected with a 61 cm-diameter 335 µm-mesh bongo net trawl down to 100 m at night. Latitude and longitude coordinates are available for all specimens (Table 1).
Table 1. Information for the Diacavolinia specimens collected, analyzed and identified for this study (by A. Maas), as well as other Cavolinia spp. sequences retrieved from GenBank.doi:10.1371/journal.pone.0053889.t001
After collection, samples were preserved in 95% ethanol which was changed once after ~24 h. All Atlantic samples were stored at –20°C to prevent DNA degradation; Pacific samples were not kept at a controlled temperature. In the lab, specimens were microscopically identified to species using the Diacavolinia key in van der Spoel et al. . Photographs were taken of each Diacavolinia species to provide later comparison. When possible, shells were removed prior to DNA extraction to avoid both the possible pH interference due to the calcium carbonate and contamination from other taxa, since the presence of some other planktonic components (mostly ostracods and copepods) inside the shell chambers was common.
DNA Extraction Procedure Tests
A series of initial tests was required to establish a reliable protocol for extraction and purification of the pteropod DNA. Three DNA purification/sample preparation kits were tested on whole individuals. Initially, extractions were carried out using DNeasy® Blood & Tissue Kit (Qiagen), with an elution volume of 200 µL in AE buffer, following the conditions established by the manufacturer with an initial digestion time of 2 h. After a number of unsuccessful PCR attempts for conserved regions on the genes COI , Cyt b  and 18S , 100 µL aliquots of five of the previous extractions were run through the OneStep™ PCR Inhibitor Removal Kit (Zymo Research Corp.), a column matrix “designed for efficient removal of polyphenolic compounds, humic/fulvic acids, tannins, melanin, etc” according to the manufacturer product information sheet. Finally, the E.Z.N.A.® Mollusc DNA Kit (Omega Bio-Tek Inc.) was applied to both new individuals and to 50 µL aliquots from the DNeasy® extractions. All E.Z.N.A.® final extractions and re-extractions were carried out following the manufacturer recommendations, with lysis incubations at 60°C for ~3 h, and a final elution on 200 µL independent of the body size of the animal.
After extraction, PCR amplification reactions were performed in a total volume of 25 µL, including 5 µL of 5× Green GoTaq® Flexi Buffer, 2.5 µL of 25 mM MgCl2, 1 µL of dNTPs (final concentration 0.2 mM each), 1 µL of each primer (10 µM), 0.75 units of GoTaq® Flexi DNA Polymerase (Promega) and 2 µL of DNA sample. PCR cycle conditions were relaxed, with annealing temperatures of 45°C/50°C/52°C for COI/Cyt b/18 S respectively. PCR products were checked by electrophoresis on a 1% agarose/TBE gel. Crossed PCR reactions on mixes of different extractions were carried out to confirm the presence of PCR inhibitors after some of the protocols.
As a result of findings from the above trials, all individuals were subsequently extracted using the E.Z.N.A.® Mollusc DNA Kit (OMEGA), following the manufacturer recommendations, with lysis incubations at 60°C for ~3 h, and a final elution on 200 µL independent of the body size of the animal.
After extraction, PCR amplification reactions for the barcoding region were performed, using M13-tailed  LCO1490 and HCO2198 universal primers for COI . The PCR protocol included an initial denaturation step of 94°C (3 min), followed by 35 cycles of denaturation at 94°C for 35 s, annealing at 45°C for 45 s, and extension at 69°C for 45 s. A final extension phase at 69°C for 15 min was followed by storage at 4°C. PCR products were checked by electrophoresis on a 1% agarose/TBE gel. PCR products were excised from the gel and purified with QIAquick Gel Extraction Kit (Qiagen). The purified PCR products were sequenced using the tailed M13 tails (both forward and reverse) and Big Dye Terminator Ver. 3.1 kit (Applied Biosystems Inc., ABI), and run on an ABI 3130 Genetic Analyzer capillary DNA sequencer. All sequences were deposited in GenBank (accession numbers JX183560-JX183616).
For comparison, additional sequences for certain Cavolinia species from Jennings et al.  were retrieved from GenBank (Table 1). No photographs are available for these samples. Note that the Jennings et al. samples include two specimens identified as Cavolinia longirostris from the Atlantic. This is an outdated identification, however, since as described above, this species has been split into a number of species and elevated to its own genus, Diacavolinia. The Jennings et al. C. longirostris is thus presumably some undetermined species of Diacavolinia.
Sequences were edited using MEGA ver. 5 , and aligned using the ClustalW  as implemented in MEGA. Parsimony haplotype networks (gene genealogies) were constructed with TCS Ver. 1.2.1 , in order to visualize the diversity and phylogenetic relationships among the different haplotypes and provide qualitative assessment of their distributions across the different individuals from the Atlantic Ocean. Haplotype diversity and Tajima’s D neutrality test were calculated with DnaSP ver. 5 .
To investigate intra-specific, inter-specific, and inter-generic relationships for Diacavolinia and Cavolinia, genetic distances were obtained following the Kimura 2-parameter (K2P) method , since this method has become the metric most widely used in barcoding studies , , . To study the differences on the distances a) within the Cavolinia genus (between species, excluding Diacavolinia), b) between the Cavolinia and Diacavolinia, and c) between the Atlantic and Pacific Diacavolinia, Mann-Whitney U tests were carried out. To reduce the probability of false positives, strict Bonferroni correction  was applied for the multiple comparisons (αcorrected = 0.017). Although there is a lack of independence among the measured genetic distances, this method has frequently been used to explore differences between taxonomic levels .
To investigate the species assignment by a monophyly criterion, a tree analysis was conducted. Trees were constructed based on Maximum Likelihood (ML) and Bayesian Inference (BI), and were carried out with RAxML Ver. 7.2.3 ,  and MrBayes Ver. 3.2  respectively. ML analysis was run under the GTR model of nucleotide substitution with the Γ model of rate heterogeneity (GTRGAMMA) and a completely random starting tree. Bootstrap support for the nodes was obtained after 10,000 replicates. BI analysis was run for 3,000,000 generations, with a sample frequency of 1000 generations. The first 500 trees were discarded as burn-in, so 2500 trees were accepted from each run. Clade support on the nodes of the trees corresponds to their Bayesian Posterior Probability (BPP), and was considered significant only when BPP>0.90.
Individuals were collected from international waters, exempting them from legislation; however, all scientific shipboard activities were conducted in such a way as to comply with the current laws of the United States of America. The study organisms are invertebrates, and as such no restrictions apply to their handling as experimental organisms.
Species Identification Based on Morphology
Using current references and accepted morphologically-based species descriptions , we identified four species of Diacavolinia from the Atlantic Ocean (72 morphologically examined and 53 successful DNA extractions of 54 attempts) and one species in the Pacific Ocean (15 morphologically examined and 3 successful DNA extractions out of 10 attempts). We documented four species from a single Reeve net tow to 100 m in the Northwest Atlantic (Table 1, Figure 1). One additional group of individuals may not have completed the transition to adult shell morphology so it has also been classified as a possible juvenile shell form. Two other sites from the same cruise collected with the MOCNESS had a similar species composition, but lower densities and diversity. It was impossible to examine the morphological features of the individuals whose sequences were taken from GenBank, and as a result the Jennings et al. individuals  could not be identified to species level and were left as Cavolinia longirostris in all further documentation and treated as Diacavolinia in our comparative analyses.
Figure 1. Diacavolinia species.
Photographs of the various shell morphologies from the Atlantic and Pacific (black box) samples and drawings of the holotypes reproduced from van der Spoel et al. . All photographs are from the ventral view except for D. robusta which is depicted from the dorsal view to show the rostral curvature. Drawings are of the ventral (left) and side (right) view of empty shells. Note that the photographs are not to scale.doi:10.1371/journal.pone.0053889.g001
Molecular Analysis: DNA Extraction, PCR, and Sequencing
PCR reactions carried out on individuals extracted with the Qiagen kit failed to amplify any product. Furthermore, the addition of 1 µl of extraction into a reaction containing a positive control (1 µL template) also resulted in failed amplifications, indicating the presence of PCR inhibitors on the extractions (Figure 2A). No improvement in success resulted from passing the extraction through the OneStep™ PCR Inhibitor Removal Kit column (Fig. 2B). On the other hand, E.Z.N.A. extractions, from both new individuals and from aliquots from the previous Quiagen extractions, all resulted in successful amplifications (Fig. 2B). After extracting all individuals with the E.Z.N.A. kit, the final PCR success rate was >98% on the recently (2011) collected samples from the Atlantic Ocean. PCR success rate on the samples from the Pacific Ocean was lower (≈30%), indicating that not only fixation technique, but also storage conditions, are critical for molecular studies of this group of taxa. The findings of these tests serve as a reminder of the importance of optimizing methods for the particular chemistry of individual animal groups and detailed methodological descriptions. We recommend the use of this extraction method for further investigations on planktonic mollusks.
Figure 2. PCR results from extraction procedure trials.
A: PCR for the COI gene on a positive control (C), two Atlantic Diacavolinia Qiagen extractions (Q1 and Q2) as well as reactions performed mixing 1 µL from the positive control and 1 µL from the same extractions as template. B: 18S gene amplification results from a Qiagen extraction (Q); Qiagen extraction after applying it through a Zymo column (QZ); E.Z.N.A. extractions (O); and E.Z.N.A. extraction on an aliquot from a Qiagen extraction (OQ). N indicates a negative control. Only E.Z.N.A. extraction showed positive PCR results, suggesting the presence of inhibitors remaining when other kits were used. Ladder for both pictures: exACTGene 1 kb Plus DNA ladder (Fisher).doi:10.1371/journal.pone.0053889.g002
A 658 base pair (bp) region was used for the definitive multiple alignment and analyses, including sequences obtained from GenBank (the alignment file is provided in File S1). All the Diacavolinia and Cavolinia sequences encoded for the same amino-acid sequence with the exception of two positions (i.e., non-synonymous mutations): one exclusive to the Diacavolinia from the Pacific Ocean (a cysteine in contrast to serine from all the others at position 98); another found in all Diacavolinia from the Atlantic and some C. uncinata (valine instead of isoleucine). All sequences and specimen metadata can be found at the corresponding GenBank records (accession numbers JX183560-JX183616).
All specimens from the Atlantic, despite distinct differences in shell morphology, showed genetic variation of <3% (K2P distance), with similar averages and ranges both within and between the different Diacavolinia species (Table 2; Figure 3). In some cases, no differences were observed between individuals from different morphospecies (the complete distance matrix file is provided in File S2). A significant deviation from neutrality was observed (Tajima’s D = −2.14, P<0.05), which could indicate an expanding population, purifying selection, or a low level of population structure , although this pattern is very common in marine animals and could also be explained by the hypothesis of sweepstakes reproductive success . The Pacific and Atlantic samples were more distant (~19%), a similar pattern to the observed differences when comparing Cavolinia uncinata from the Atlantic and Indian Ocean [~11%, Figure 3; 26]. Based on these results, Pacific Ocean samples were excluded from the gene genealogy analysis where the TCS haplotype network diagram showed no discrimination between any of the species analyzed on the network, a high number of unique haplotypes (haplotype diversity, Hd = 0.993±0.006), and very few haplotypes shared by more than one individuals (Figure 4).
Figure 3. Heatmap of pair-wise K2P genetic distances.
This heatmap depicts the genetic distances between each sampled individual based on the mitochondrial COI gene. Distances between specimens of the same species are outlined by black squares.doi:10.1371/journal.pone.0053889.g003
Figure 4. Haplotype network of Atlantic Diacavolinia species.
This haplotype network depicts the variation within the COI region of the Atlantic Diacavolinia species. Each branch represents a mutational step, and small black circles depict the missing haplotypes needed to connect observed sequences. The size of the ovals is proportional to the number of sampled individuals with that haplotype. There is no species-related clustering among haplotypes.doi:10.1371/journal.pone.0053889.g004
Table 2. Average, standard deviation, maximum and minimum K2P distances; within (w/i) the species Diacavolinia elegans (e.), strangulata (s.), juveniles/aspina (j.), atlantica (a.), and robusta (r.); between the five Diacavolinia spp. from the Atlantic (A.), within Diacavolinia vanutrechti from the Pacific (P.), between Atlantic and Pacific individuals of the Diacavolinia, and between all Diacavolinia and Cavolinia spp.doi:10.1371/journal.pone.0053889.t002
Comparisons of Diacavolinia spp. with Cavolinia spp. reveal larger distances (~24%). Statistically, genetic distances showed a much higher average when comparing Diacavolinia spp. to Cavolinia spp. than within each genus (p<0.001 in both comparisons; Table 2, Figure 5). Distances between species of Cavolinia were significantly higher than distances between the Atlantic and Pacific populations of Diacavolinia (p<0.01; Figure 5).
Figure 5. Distribution of the K2P distances between and within Diacavolinia and Cavolinia species.
Box-Whisker plot showing the minimum, maximum, median, lower quartile, and upper quartile of K2P distances comparing Diacavolinia to Cavolinia spp., Atlantic to Pacific Diacavolinia individuals, and among Cavolinia species.doi:10.1371/journal.pone.0053889.g005
Trees showed consistency between both the Maximum Likelihood and Bayesian Inference methods, revealing the polyphyly of the Atlantic morphologically defined species(Figure 6). All Diacavolinia individuals from the Atlantic (both from this study and from GenBank) were clustered in a single node, without any morphology-related pattern of discrimination within the clade. Some smaller sub-clades of these sequences were statistically supported, but these often contained individuals belonging to different Diacavolinia species. At a genus level, Diacavolinia appeared as monophyletic: the Pacific Ocean individuals, identified via the morphological key as D. vanutrechti, clustered in a monophyletic sister clade to the Atlantic Diacavolinia spp. Very low distances were evident within the Atlantic and Pacific clades, whereas much longer branches connected the two nodes. In our tree analyses Diacavolinia spp. were a significantly distinct branch of the Cavoliniinae. The rest of the subfamily cluster showed Cavolinia globulosa and Cavolinia tridentata associated together in a separate clade from Cavolinia uncinata. Cavolinia uncinata were represented by two distinct groupings and were closely associated with Cavolinia gibbosa.
Figure 6. Tree analysis of the Diacavolinia spp. examined in this study and Cavoliniid sequences retrieved from GenBank.
Topology and branch lengths reflect the tree with the best score under the Maximum Likelihood criteria (in RAxML). Numbers at nodes indicate the percentage bootstrap recovery and the Bayesian Posterior Probability of that node. All Diacavolinia from the Atlantic Ocean were recovered in a monophyletic clade, with no morphology–related subdivisions. Diacavolinia vanutrechti were shown as monophyletic, and distinct to the Diacavolinia from the Atlantic.doi:10.1371/journal.pone.0053889.g006
Our results suggest that the designation of these forms by van der Spoel et al.  as separate species is likely inappropriate. Despite distinct differences in shell morphology that were the basis of the original species descriptions, there were no significant differences between the four different morphological forms of Atlantic Diacavolinia studied in both tree and distance-based analyses. There are differences, however, in Diacavolinia spp. on a basin scale with an approximately ten times higher distance in the between-basin, also shown in the tree analyses, consistent with the presence of a species-related barcode gap , . The differences between the Pacific and Atlantic Diacavolinia sequences, suggestive of species level distinctions between populations, are similar to those previously reported between congeneric species in pteropods , although high differences within the same species between ocean basins have been reported for many holoplanktonic taxa , , , , . Overall, these findings indicate that some of the species identifications established by van der Spoel et al.  should be reconsidered, although any renaming and reclassifying of species will need to await the collection of more samples from a broader geographic distribution for genetic analysis of all of van der Spoel’s 22 putative species. In contrast, the high genetic distances between the genera Diacavolinia and Cavolinia as well as the unique reproductive structures and locking mechanism described by van der Spoel , would support the persistence of Diacavolinia as a separate genus. For the Cavolinia species retrieved from GenBank for comparison and framing the genera, our results were consistent with those obtained and discussed by Jennings et al. .
Recent tests of the effect of spatial and numerical coverage on barcode efficacy for resolving patterns in species identification emphasize the importance of large sample size (ranging from at least 150-50 individuals per species) and an awareness of changes in the ability of software to recognize a barcode gap at larger geographic scales , , . As our Diacavolinia sampling was only at four locations, three in a relatively constrained region of the NW Atlantic Ocean, and since we had a somewhat limited number of individuals, particularly in the Pacific, it is likely that further sampling would change the fine details of the pattern we have documented. The pronounced barcode gap would probably decrease in size with increased distributional coverage and sample size, and the diversity in the Pacific group would increase. However, the genetic distances between the Atlantic and Pacific populations of Diacavolinia are larger than most previously documented populations from the same planktonic species , , , even those that exist in multiple ocean basins. We feel, therefore, that greater sampling would not change our central conclusions and our findings are minimally suggestive that existing species delimitations should be re-visited.
The differences in shell morphology within the Atlantic Diacavolinia, the monophyletic recovery of all the individuals without segregation among the different species, and the low K2P distances in their COI sequence (<3%) suggest a high level of phenotypic variation in regard to shell morphology within the species. Although in their various studies, van der Spoel and colleagues frequently found sympatry of shell morphologies, it was concluded that these differences were a result of genetic variation. Alternate explanations include a shell form which is not under strong selective pressure or a shell form that is influenced by differences in life history and developmental environment, as was previously suggested by McGowan . One clue to the possible mechanism by which the shell shape of these animals could be influenced by environment involves the development of the adult teloconch in the Cavoliniinae subfamily. Although often overlooked, it has been documented in the literature that individuals of this group develop their adult shell in a unique way. The adult teloconch is rapidly extended from the somewhat flattened and curved conical juvenile protoconch. When the teloconch reaches a large size the growing animal extrudes its mantle to surround the shell, decalcifies the structure and then rapidly mechanically increases the shell volume and recalcifies the shell in the characteristically bulging adult shape, then loses the juvenile protoconch . All further growth is predominantly in the soft parts, although extensions of the rostrum and lateral spines or thickening of the shell may continue throughout life, a fact that may result in individuals with similar length shells containing animals of varying age, mantle size, and overall mass. This relationship between overall mass and shell length was found by Gilmer , although the mechanism at that time was not discussed. This demineralization process has also been documented in Cavolinia uncinata and may produce a similar variation in shell morphology. If disparities in shell shape, which have been used to designate forma in Cavolinia uncinata, are similarly exclusively a result of developmental variation, this could explain the lack of genetic support for their differentiation found in Jennings et al. . The decalcification and recalcification of the shell, and the energetic investment available for the deformation may be dependent on food availability, physiological state, water temperature and environmental carbonate chemistry. Variations in any of these factors might result in profound differences in shell angle and size, which could explain the sympatry of shell forms. This developmental mechanism bears further investigation, particularly as the carbonate chemistry of the ocean changes in response to anthropogenic forcing. The sensitivity of this group of thecosomatous pteropods to ocean acidification may be impacted by this phenotypic variation and their control over calcification.
Our results have a number of implications for biodiversity, ecology, and population resiliency in the face of changing oceanic conditions. The species level differences between Diacavolinia from the Pacific and Atlantic Oceans in this study are similar to the regional differences in other Cavolinid species, including Cavolinia uncinata, Cuvierina columnella, Diacria major, and Clio cuspidata documented by Jennings et al. . These findings suggest that further investigations of Indian Ocean, Red Sea and Southern Hemisphere populations of Diacavolinia spp. may reveal a number of regional species. It is important to investigate such groups to determine their taxonomic differences, as there may be functional variability in the populations. This is particularly important with regards to studies of their sensitivity to changing environmental conditions, as there are ocean basin differences in hydrography that may result in different natural exposures and subsequently different physiological sensitivities to stressful conditions. For example, individuals of the Pacific population of Diacavolinia, although they were identified as Cavolinia longirostris in previous studies, are known to undergo a diel vertical migration into an oxygen minimum zone, where the water is thought to be undersaturated with respect to aragonite, pH is ~7.5, and oxygen is well below 20 µM O2 kg−1 , , . This oxygen minimum/carbon maximum zone is extensive in the Pacific Ocean, whereas similar conditions are absent from the Atlantic . Individuals of Diacavolinia from the Pacific were not responsive to short term laboratory exposure to conditions of elevated carbon dioxide (~1000 ppm); however, since this population is genetically distinct from the Atlantic, as indicated by this study, then it is possible that their physiological responses may be different as well, and the Atlantic individuals could be more sensitive to enhanced carbon dioxide. As an indicator, the single mutation that is exclusive to the Pacific Diacavolinia (cysteine instead of serine) might not be trivial, since cysteines are the ligand points for the copper units in the cytochrome c oxidase complex , and they also are known to be regulation points in other oxidases , . Subsequently, this difference in the COI sequence may influence the efficiency of the respiratory chain and therefore the sensitivity of these populations of animals to oxygen concentration and internal pH. Having accurate identifications of species, together with an understanding of their basin scale distribution and biodiversity, could therefore be critical for making informed estimates of planktonic ecosystem sensitivity to anthropogenic change.
File containing the aligned 658 base pair (bp) COI region for Cavoliniinae from this study and from Genbank.
Distance matrix (K2P) for the Cavoliniinae from this study and from Genbank.
We would like to acknowledge the expertise and assistance of the Captain and Crew of the R/V Oceanus and to thank all of the scientists and students who assisted with the 2011 OC473 cruise as well as co-PIs Andone Lavery, Aleck Wang, and Peter Wiebe. We are grateful to Brad Seibel for permitting the use of samples collected in the Pacific Ocean in 2007. We would like to thank Ann Bucklin, Peter Wiebe, Nancy Copley and Michael Finiguerra for their support, insight and input into methodologies, analysis and interpretation. The UConn Bioinformatics Facility provided computing resources for the Bayesian and maximum likelihood phylogenetic analyses performed for this study.
Conceived and designed the experiments: AEM LBB GLL. Performed the experiments: AEM LBB. Analyzed the data: AEM LBB. Contributed reagents/materials/analysis tools: LBB GLL. Wrote the paper: AEM LBB GLL.
- 1. Fabry VJ, Seibel BA, Feely RA, Orr JC (2008) Impacts of ocean acidification on marine fauna and ecosystem processes. ICES Journal of Marine Science 65: 414–432. doi: 10.1093/icesjms/fsn048
- 2. Comeau S, Gorsky G, Jeffree R, Teyssie J, Gattuso JP (2009) Impact of ocean acidification on a key Arctic pelagic mollusc (Limacina helicina). Biogeosciences 6: 1877–1882. doi: 10.1093/icesjms/fsn048
- 3. Comeau S, Gorsky G, Alliouane S, Gattuso JP (2010b) Larvae of the pteropod Cavolinia inflexa exposed to aragonite undersaturation are viable but shell-less. Marine Biology 157: 2341–2345. doi: 10.1093/icesjms/fsn048
- 4. Lischka S, Büdenbender J, Boxhammer T, Riebesell U (2011) Impact of ocean acidification and elevated temperatures on early juveniles of the polar shelled pteropod Limacina helicina: mortality, shell degradation, and shell growth. Biogeosciences 13: 919–932. doi: 10.1093/icesjms/fsn048
- 5. Comeau S, Jeffree R, Teyssié JL, Gattuso JP (2010a) Response of the Arctic pteropod Limacina helicina to projected future environmental conditions. PLoS ONE 5: e11362. doi: 10.1371/journal.pone.0011362
- 6. Maas AE, Elder LE, Dierssen HM, Seibel BA (2011) Metabolic response of Antarctic pteropods (Mollusca: Gastropoda) to food deprivation and regional productivity. Marine Ecology Progress Series 441: 129–139. doi: 10.3354/meps09358
- 7. Seibel BA, Maas AE, Dierssen HM (2012) Energetic plasticity underlies a variable response to ocean acidification in the pteropod, Limacina helicina antarctica. PLoS ONE 7: e30464. doi: 10.1371/journal.pone.0030464
- 8. Hunt BPV, Pakhomov EA, Hosie GW, Siegel V, Ward P, et al. (2008) Pteropods in Southern Ocean ecosystems. Progress in Oceanography 78: 193–221. doi: 10.3354/meps09358
- 9. Lalli CM, Gilmer RW (1989) Pelagic Snails: The Biology of Holoplanktonic Gastropod Mollusks. Stanford, CA: Stanford University Press.
- 10. Pakhomov EA, Froneman PW, Wassmann P, Ratkova T, Arashkevich E (2002) Contribution of algal sinking and zooplankton grazing to downward flux in the Lazarev Sea (Southern Ocean) during the onset of phytoplankton bloom: a lagrangian study. Marine Ecology Progress Series 233: 73–88. doi: 10.3354/meps09358
- 11. Bernard KS, Froneman PW (2009) The sub-Antarctic euthecosome pteropod, Limacina retroversa: Distribution patterns and trophic role. Deep Sea Research Part I: Oceanographic Research 56: 582–598. doi: 10.1016/j.dsr.2008.11.007
- 12. Bernard KS, Steinberg DK, Schofield OME (2012) Summertime grazing impact of the dominant macrozooplankton off the Western Antarctic Peninsula. Deep Sea Research Part I: Oceanographic Research Papers 62: 111–122. doi: 10.1016/j.dsr.2008.11.007
- 13. Noji TT, Bathmann UV, Bodungen B, Voss M, Antia A, et al. (1997) Clearance of picoplankton-sized particles and formation of rapidly sinking aggregates by the pteropod, Limacina retroversa. Journal of Plankton Research 19: 863–875. doi: 10.1016/j.dsr.2008.11.007
- 14. Honjo S (2004) Particle export and the biological pump in the Southern Ocean. Antarctic Science 16: 501–516. doi: 10.1016/j.dsr.2008.11.007
- 15. Bauerfeind E, NÃthig EM, Beszczynska A, Fahl K, Kaleschke L, et al. (2009) Particle sedimentation patterns in the eastern Fram Strait during 2000–2005: Results from the Arctic long-term observatory HAUSGARTEN. Deep Sea Research Part I: Oceanographic Research Papers 56: 1471–1487. doi: 10.1016/j.dsr.2008.11.007
- 16. Manno C, Tirelli V, Accornero A, Fonda Umani S (2010) Importance of the contribution of Limacina helicina faecal pellets to the carbon pump in Terra Nova Bay (Antarctica). Journal of Plankton Research 32: 145–152. doi: 10.1093/plankt/fbp108
- 17. Gilmer RW, Harbison GR (1991) Diet of Limacina helicina (Gastropoda: Thecosomata) in Arctic waters in midsummer. Marine Ecology Progress Series 77: 125–134. doi: 10.1093/plankt/fbp108
- 18. Falk-Petersen S, Sargent JR, Kwasniewski S, Gulliksen B, Millar RM (2001) Lipids and fatty acids in Clione limacina and Limacina helicina in Svalbard waters and the Arctic Ocean: Trophic implications. Polar Biology 24: 163–170. doi: 10.1093/plankt/fbp108
- 19. Karnovsky NJ, Hobson KA, Iverson S, Hunt GL (2008) Seasonal changes in diets of seabirds in the North Water Polynya: a multiple-indicator approach. Marine Ecology Progress Series 357: 99. doi: 10.1093/plankt/fbp108
- 20. Foster BA, Cargill JM, Montgomery JC (1987) Planktivory in Pagothenia borchgrevinki (Pisces: Nototheniidae) in McMurdo Sound, Antarctica. Polar Biology 8: 49–54. doi: 10.1093/plankt/fbp108
- 21. Armstrong JL, Boldt JL, Cross AD, Moss JH, Davis ND, et al. (2005) Distribution, size, and interannual, seasonal and diel food habits of northern Gulf of Alaska juvenile pink salmon, Oncorhynchus gorbuscha. Deep Sea Research Part II: Topical Studies in Oceanography 52: 247–265. doi: 10.1016/j.dsr2.2004.09.019
- 22. Somero GN (2010) The physiology of climate change: how potentials for acclimatization and genetic adaptation will determine ‘winners’ and ‘losers’. The Journal of Experimental Biology 213: 912–920. doi: 10.1242/jeb.037473
- 23. Sunday JM, Crim RN, Harley CDG, Hart MW (2011) Quantifying rates of evolutionary adaptation in response to ocean acidification. PLoS ONE 6: e22881. doi: 10.1371/journal.pone.0022881
- 24. Lohbeck KT, Riebesell U, Reusch TBH (2012) Adaptive evolution of a key phytoplankton species to ocean acidification. Nature Geoscience 5: 346–351. doi: 10.1016/j.dsr2.2004.09.019
- 25. Klussmann-Kolb A, Dinapoli A (2006) Systematic position of the pelagic Thecosomata and Gymnosomata within Opisthobranchia (Mollusca, Gastropoda)–revival of the Pteropoda. Journal of Zoological Systematics & Evolutionary Research 44: 118–129. doi: 10.1016/j.dsr2.2004.09.019
- 26. Jennings RM, Bucklin A, Ossenbrügger H, Hopcroft RR (2010) Species diversity of planktonic gastropods (Pteropoda and Heteropoda) from six ocean regions based on DNA barcode analysis. Deep Sea Research Part II: Topical Studies in Oceanography 57: 2199–2210. doi: 10.1016/j.dsr2.2010.09.022
- 27. van der Spoel S, Dadon JR (1999) Pteropoda. In: Boltovskoy D, editor. South Atlantic Zooplankton. Leiden, The Netherlands: Backhuys Publishers. 649–706.
- 28. Gilmer RW (1974) Some aspects of feeding in thecosomatous pteropod molluscs. Journal of Experimental Marine Biology and Ecology 15: 127–144. doi: 10.1016/j.dsr2.2010.09.022
- 29. Hunt B, Strugnell J, Bednarsek N, Linse K, Nelson RJ, et al. (2010) Poles Apart: The “Bipolar” Pteropod Species Limacina helicina Is Genetically Distinct Between the Arctic and Antarctic Oceans. PLoS ONE 5: e9835. doi: 10.1371/journal.pone.0009835
- 30. van der Spoel S (1987) Diacavolinia nov. gen. separated from Cavolinia (Pteropoda, Gastropoda). Bull zool Mus Univ Amsterdam 11: 77–80. doi: 10.1016/j.dsr2.2010.09.022
- 31. Van der Spoel S, Bleeker J, Kobayashi H (1993) From Cavolinia longirostris to twenty-four Diacavolinia taxa, with a phylogenetic discussion (Mollusca, Gastropoda). Bijdragen tot de Dierkunde 62: 127–166.
- 32. van der Spoel S (1968) The shell and its shape in Cavoliniidae (Pteropoda, Gastropoda). Beaufortia Bulletin Zoological Museum 16.
- 33. Newman LJ (1990) Holoplanktonic molluscs (Gastropoda; Thecosomata, Gymnosomata and Heteropoda) from the waters of Australia and Papua New Guinea: Their taxonomy, distribution and biology. Brisbane: University of Queensland. 208 p.
- 34. de Blainville H (1821) Malacoz. Dictionnaire des Sciences naturelles 22: 1–570.
- 35. Tesch JJ (1946) The Thecosomatous Pteropods: I. The Atlantic. Copenhagen: Carlsberg Foundation. 82 p.
- 36. Tesch JJ (1948) The Thecosomatous Pteropods: II. The Indo-Pacific: A. Høst.
- 37. van der Spoel S (1971) New forms of Diacria quadridentata (de Blainville, 1821) Cavolinia longirostris (de Blainville, 1821) and Cavolinia uncinata (Rang, 1829) from the Red Sea and the East Pacific Ocean (Mollusca, Pteropoda). Beaufortia 19: 1–20.
- 38. van der Spoel S (1970) Morphometric data on Cavoliniidae, with notes on a new form of Cuvierina columnella (Rang, 1827)(Gastropoda, Pteropoda). Basteria 33: 103–151.
- 39. van der Spoel S (1973) Variation in Cavolinia longirostris (de Blainville, 1821) from the Pacific Ocean with discription of a newforma (Mollusca, Pteropoda). Bull zool Mus Univ Amsterdam 3: 99–102.
- 40. McGowan JA (1960) The systematics, distribution and abundance of the Euthecosomata of the North Pacific: University of California, San Diego. 197 p.
- 41. Hebert PDN, Ratnasingham S, deWaard JR (2003) Barcoding animal life: cytochrome c oxidase subunit I divergences among closely related species. Proceedings of the Royal Society B: Biological Sciences 270: S96–S99. doi: 10.1098/rsbl.2003.0025
- 42. Bucklin A, Steinke D, Blanco-Bercial L (2011) DNA Barcoding of marine Metazoa. Annual Review of Marine Science 3: 471–508. doi: 10.1098/rsbl.2003.0025
- 43. Remigio EA, Hebert PDN (2003) Testing the utility of partial COI sequences for phylogenetic estimates of gastropod relationships. Molecular Phylogenetics and Evolution 29: 641–647. doi: 10.1016/S1055-7903(03)00140-4
- 44. Will KW, Rubinoff D (2004) Myth of the molecule: DNA barcodes for species cannot replace morphology for identification and classification. Cladistics 20: 47–55. doi: 10.1098/rsbl.2003.0025
- 45. DeSalle R, Egan MG, Siddall M (2005) The Unholy Trinity: taxonomy, species delimitation and DNA Barcoding. Philosophical Transactions: Biological Sciences 360: 1905–1916. doi: 10.1098/rstb.2005.1722
- 46. Rubinoff D (2006) DNA Barcoding evolves into the familiar. Conservation Biology 20: 1548–1549. doi: 10.1111/j.1523-1739.2006.00542.x
- 47. Köhler F (2007) From DNA taxonomy to barcoding - how a vague idea evolved into a biosystematic tool. Mitteilungen aus dem Museum für Naturkunde in Berlin - Zoologische Reihe 83: 44–51. doi: 10.1002/mmnz.200600025
- 48. Wiebe P, Morton A, Bradley A, Backus R, Craddock J, et al. (1985) New development in the MOCNESS, an apparatus for sampling zooplankton and micronekton. Marine Biology 87: 313–323. doi: 10.1002/mmnz.200600025
- 49. Folmer O, Black M, Hoeh W, Lutz R, Vrijenhoek R (1994) DNA primers for amplification of mitochondrial cytochrome c oxidase subunit I from diverse metazoan invertebrates. Molecular Marine Biology and Biotechnology 3: 294–299. doi: 10.1002/mmnz.200600025
- 50. Merritt TJS, Shi L, Chase MC, Rex MA, Etter RJ, et al. (1998) Universal cytochrome b primers facilitate intraspecific studies in molluscan taxa. Molecular Marine Biology and Biotechnology 7: 7–11. doi: 10.1002/mmnz.200600025
- 51. Zhang H, Lin S (2002) Detection and quantification of Pfiesteria piscicida by using the mitochondrial Cytochrome b gene. Applied and Environmental Microbiology 68: 989–994. doi: 10.1128/AEM.68.2.989-994.2002
- 52. Messing J (1983) New M13 vectors for cloning. Methods in Enzymology 101: 20–78. doi: 10.1016/0076-6879(83)01005-8
- 53. Tamura K, Peterson D, Peterson N, Stecher G, Nei M, et al. (2011) MEGA5: Molecular Evolutionary Genetics Analysis using maximum likelihood, evolutionary distance, and maximum parsimony methods. Molecular Biology and Evolution 28: 2731–2739. doi: 10.1093/molbev/msr121
- 54. Thompson JD, Higgins DG, Gibson TJ (1994) CLUSTAL W: improving the sensitivity of progressive multiple sequence alignment through sequence weighting, position-specific gap penalties and weight matrix choice. Nucleic Acids Research 22: 4673–4680. doi: 10.1093/nar/22.22.4673
- 55. Clement M, Posada D, Crandall KA (2000) TCS: a computer program to estimate gene genealogies. Molecular Ecology 9: 1657–1659. doi: 10.1046/j.1365-294x.2000.01020.x
- 56. Librado P, Rozas J (2009) DnaSP v5: a software for comprehensive analysis of DNA polymorphism data. Bioinformatics 25: 1451–1452. doi: 10.1093/bioinformatics/btp187
- 57. Kimura M (1980) A simple method for estimating evolutionary rates of base substitutions through comparative studies of nucleotide sequences. Journal of molecular evolution 16: 111–120. doi: 10.1007/BF01731581
- 58. Matzen da Silva J, Creer S, Dos Santos A, Costa AC, Cunha MR, et al. (2011) Systematic and Evolutionary Insights Derived from mtDNA COI Barcode Diversity in the Decapoda (Crustacea: Malacostraca). PLoS ONE 6: e19449. doi: 10.1371/journal.pone.0019449
- 59. Bonferroni CE (1936) Teoria statistica delle classi e calcolo delle probabilità. Pubblicazioni del R Istituto Superiore di Scienze Economiche e Commerciali di Firenze 8: 3–62.
- 60. Stamatakis A (2006) RAxML-VI-HPC: maximum likelihood-based phylogenetic analyses with thousands of taxa and mixed models. Bioinformatics 22: 2688–2690. doi: 10.1093/bioinformatics/btl446
- 61. Ott M, Zola J, Stamatakis A, Aluru S (2007) Large-scale maximum likelihood-based phylogenetic analysis on the IBM BlueGene/L. Proceedings of the 2007 ACM/IEEE conference on Supercomputing. Reno, Nevada: ACM. 1–11.
- 62. Ronquist F, Teslenko M, van der Mark P, Ayres DL, Darling A, et al. (2012) MrBayes 3.2: efficient bayesian phylogenetic inference and model choice across a large model space. Systematic Biology 61: 539–542. doi: 10.1093/sysbio/sys029
- 63. Tajima F (1989) Statistical method for testing the neutral mutation hypothesis by DNA polymorphism. Genetics 123: 585–595.
- 64. Hedgecock D, Pudovkin AI (2011) Sweepstakes Reproductive Success in highly fecund marine fish and shellfish: a review and commentary. Bulletin of Marine Science 87: 971–1002.
- 65. Hebert PD, Stoeckle MY, Zemlak TS, Francis CM (2004) Identification of birds through DNA barcodes. PLoS Biology 2: E312. doi: 10.1371/journal.pbio.0020312
- 66. Blanco-Bercial L, Álvarez-Marqués F, Bucklin A (2011) Comparative phylogeography and connectivity of sibling species of the marine copepod Clausocalanus (Calanoida). Journal of Experimental Marine Biology and Ecology 404: 108–115.
- 67. Goetze E (2003) Cryptic speciation on the high seas; global phylogenetics of the copepod family Eucalanidae. Proceedings of the Royal Society B: Biological sciences 270: 2321–2331.
- 68. Eberl R, Cohen S, Cipriano F, Carpenter EJ (2007) Genetic diversity of the pelagic harpacticoid copepod Macrosetella gracilis on colonies of the cyanobacterium Trichodesmium spp. Aquatic Biology 1: 33–43.
- 69. Miyamoto H, Machida RJ, Nishida S (2010) Genetic diversity and cryptic speciation of the deep sea chaetognath Caecosagitta macrocephala (Fowler, 1904). Deep Sea Research Part II: Topical Studies in Oceanography 57: 2211–2219.
- 70. Bergsten J, Bilton DT, Fujisawa T, Elliott M, Monaghan MT, et al. (2012) The effect of geographical scale of sampling on DNA barcoding. Systematic Biology 61: 851–869. doi: 10.1093/sysbio/sys037
- 71. Goetze E (2010) Species discovery in marine planktonic invertebrates through global molecular screening. Molecular Ecology 19: 952–967. doi: 10.1111/j.1365-294X.2009.04520.x
- 72. Zhang A, He L, Crozier R, Muster C, Zhu CD (2010) Estimating sample sizes for DNA barcoding. Molecular Phylogenetics and Evolution 54: 1035–1039. doi: 10.1016/j.ympev.2009.09.014
- 73. Bandel K, Hemleben C (1995) Observations on the ontogeny of thecosomatous pteropuds (holoplanktic Gastropoda) in the southern Red Sea and from Bermuda. Marine Biology 124: 225–243. doi: 10.1007/bf00347127
- 74. Paulmier A, Ruiz-Pino D, Garçon V (2011) CO2 maximum in the oxygen minimum zone (OMZ). Biogeosciences 8: 239–252. doi: 10.1007/bf00347127
- 75. Maas AE, Wishner KF, Seibel BA (2012) The metabolic response of pteropods to acidification reflects natural CO2-exposure in oxygen minimum zones. Biogeosciences 9: 747–757. doi: 10.1007/bf00347127
- 76. Maas AE, Wishner KF, Seibel BA Metabolic suppression in thecosomatous pteropods as an effect of low temperature and hypoxia in the Eastern Tropical North. Marine Biology in press.
- 77. Tsukihara T, Aoyama H, Yamashita E, Tomizaki T, Yamaguchi H, et al. (1995) Structures of metal sites of oxidized bovine heart cytochrome c oxidase at 2.8 Å. Science 269: 1069–1074. doi: 10.1126/science.7652554
- 78. Umbach AL, Ng VS, Siedow JN (2006) Regulation of plant alternative oxidase activity: A tale of two cysteines. Biochimica et Biophysica Acta (BBA) - Bioenergetics 1757: 135–142. doi: 10.1016/j.bbabio.2005.12.005
- 79. Babior BM (2002) The activity of leukocyte NADPH oxidase: regulation by p47PHOX cysteine and serine residues. Antioxidants & Redox Signaling 4: 35–38. doi: 10.1089/152308602753625834