Biodiversity Data Journal :
Taxonomic Paper
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Corresponding author: Camila Arnés-Urgellés (kmiarnes@gmail.com)
Academic editor: Tin-Yam Chan
Received: 19 May 2020 | Accepted: 06 Aug 2020 | Published: 03 Sep 2020
© 2020 Camila Arnés-Urgellés, Salome Buglass, Shane Ahyong, Pelayo Salinas-de-León, Mary Wicksten, Leigh Marsh
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Arnés-Urgellés C, Buglass S, Ahyong ST, Salinas-de-León P, Wicksten MK, Marsh L (2020) Arthropoda; Crustacea; Decapoda of deep-sea volcanic habitats of the Galapagos Marine Reserve, Tropical Eastern Pacific. Biodiversity Data Journal 8: e54482. https://doi.org/10.3897/BDJ.8.e54482
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The deep-sea biome (> 200 m depth) is the world’s last great wilderness, covering more than 65% of the earth’s surface. Due to rapid technological advances, deep-sea environments are becoming more accessible to scientific research and ocean exploration around the world and, in recent years, this is also true for the Galapagos Islands. Deep-sea habitats cover the largest proportion of Galapagos Marine Reserve (GMR), yet to date, no comprehensive baseline exists on the biodiversity of the benthic fauna associated with volcanic seafloor formations within this region. Closing this knowledge gap is essential to provide information for decision-making for the management of marine resources within the GMR and assessing any potential changes in biodiversity resulting from climate-driven alterations that deep-sea environments are expected to experience. In 2015, the Charles Darwin Foundation’s Seamounts of the GMR Research Project, together with the Galapagos National Park Directorate (GNPD) and Ocean Exploration Trust (OET), conducted a joint expedition on board the EV Nautilus. Using Remotely operated vehicles (ROVs), the aim of the expedition was to characterise the geological formations and biological communities present on seamounts, lava flows and other deep-sea habitats (> 200 m) within the GMR.
We provide the first comprehensive image inventory for the phylum Arthropoda from 260 to 3400 m of depth within the GMR. Past studies on deep-sea macroinvertebrates in the GMR have been limited to voucher samples collected from dredging (restricted to soft bottom environments) or by submersibles (only allowing limited biological sampling). The image inventory, presented here, is based on high-definition video transects conducted by the Hercules ROV on board the EV Nautilus. Images of macroinvertebrate morphospecies were captured, catalogued and identified, thus providing the first known image inventory of in-situ macroinvertebrate species from the deep-sea region of the GMR.
We present 32 distinct morphospecies occurrences within the class Malacostraca and order Decapoda. We also report 17 different families, three species that are new records to the GMR, in-situ images of two new species to science recently described and one possible new squat lobster, as well as interesting behavioural observations.
Deep-sea, Galapagos Marine Reserve, macroinvertebrate, Arthropoda, seamounts, volcanic seascapes
The Galapagos archipelago is a volcanic island chain located in the Tropical Eastern Pacific, south of the Galapagos Spreading Center and forms part of the western end of the Carnegie Ridge (
The Galapagos Marine Reserve (GMR) covers approximately 138,000 km2 and was established in 1998 (Fig.
In recent decades, the use of Remotely operated vehicles (ROVs), equipped with effective sampling gear and high-resolution recording technologies, has greatly accelerated exploration and surveying of deep-sea habitats (
Being the first organisms to colonise the islands, even before the appearance of macroscopic plants, the terrestrial arthropods from the Galapagos Islands have been a subject of interest for many years (
Study sites
In June 2015, the EV Nautilus conducted a 10-day collaborative research expedition (NA064) between the Ocean Exploration Trust (OET), the Charles Darwin Foundation (CDF) and the Galapagos National Park Directorate (GNPD) to explore the deep-sea environments of the GMR. All methods were carried out in accordance with relevant guidelines and regulations by the GNPD under research permits PC-26-15 & PC-45-15. All experimental protocols were reviewed and approved by a GNPD’s committee which evaluates animal care during research activities. We conducted a total of six exploratory dives to the far north, west and central part of the Galapagos archipelago (Fig.
Dive |
Geographical location |
Feature |
Depth range (m) |
ROV Bottom time |
Latitude, Longitude |
H1435 |
East of Wolf |
Seamount |
1120-290 |
16 h 48 |
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H1436 |
East of Darwin |
Seamount |
2090-930 |
11 h 14 |
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H1440 |
North of Darwin |
Seamount |
1960-1190 |
11 h 21 |
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H1441 |
West of Fernandina |
Lava flows |
3370-3300 |
13 h 34 |
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H1442 |
West of Fernandina |
Lava flows |
3010-2940 |
18 h 25 |
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H1443 |
West of Santiago |
Seamount |
640-250 |
18 h 16 |
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ROV dives began at the base of each feature and conducted a general upslope transect, following sonar and visual surveys along this transect. Dives H1435, H1436 and H1440 explored three seamounts around the most northern islands of the archipelago, which are part of the Wolf-Darwin volcanic lineament that extends to the Galapagos Spreading Center (
The final dive, H1443, explored two small conically-shaped shallow seamounts located in the central part of the Archipelago, between the islands of Santiago and Isabela. Seamounts from this part of the platform were once centred over the hotspot and are estimated to be between 5 to 6 million years old (
ROV operations
Seafloor exploration was carried out using the two-body ROV system, Argus and Hercules, each rated to 4000 m water depth. Video and still images of the sites were taken using "Insite Pacific Zeus Plus" HD colour video cameras on both vehicles, each equipped with a 10× mechanical zoom lens. All in-situ images used for the inventory were obtained by Hercules’ mounted camera system. Additionally, environmental parameters were also recorded using Hercules’ telemetry sensors, which included oxygen concentration (Aanderaa Oxygen Optode 3830), temperature and salinity (Seabird FastCat 49Plus).
While the majority of the species analysed for this study were identified from image only, a few specimens were opportunistically collected using the ROV’s hydraulic manipulators. After recovery of the ROV, the collected specimens were preserved following standardised protocols and this information is specified in the 'preparations' and 'notes' sections for each organism listed on the species checklist below.
Video transects image analysis
Each ROV dive ranged in duration from 11 to 18 hours. For the subsequent review of morphospecies, each dive was spilt into 2-hour segments. In-situ images of organisms were captured and extracted from video transects analyses using VLC software (Version 3.0.4) by “non-expert analysts”. To avoid reviewer bias in capturing unique morphospecies, five “non-expert analysts” were assigned random video segments from all six ROV dives. Only organisms that appear to be larger than 3 cm were captured and considered for further identification. All images were then tentatively classified under their common names (i.e. squat lobsters, crabs, shrimps, etc.) and only images that appeared in sufficient detail to be determined beyond phyla were sent to taxonomic experts for further identification. Taxonomists identified all images to the lowest taxonomic level possible. To identify the species, taxonomists consulted published literature (e.g.
The open nomenclature identification qualifiers presented here are modified from
Below is a brief overview of each qualifier assigned to the different Arthropoda morphospecies. We assigned the qualifier, based on the original comments provided by each taxonomist.
indet. (indeterminabilis) The sign 'indet.' is to be used as an abbreviation of indeterminabilis and to indicate that the specimen is indeterminable beyond a certain taxonomic level due to the lack of diagnostic characters visible in the image. This qualifier can also be used at higher taxonomic ranks and in conjunction with inc. (below) to indicate a difference between the uncertainties of the IDs at higher taxonomic ranks. We also used this term for some of the very poor-quality images.
inc. (incerta) the usage of this qualifier is to be restricted to the meaning of 'uncertain identification' and to be equated to the question mark. Since the latter may be considered as a 'wildcard' by some software, in data stored in digital form, it may be substituted by 'sp. inc.', 'gen. inc.' etc.
stet. (stetit) Use the term stetit after the taxon name to explicitly express the identifier choice of not proceeding further.
A total of 32 distinct morphospecies of arthropods were identified, belonging to 17 families, 19 genera and 13 confirmed species of the class Malacostraca, order Decapoda.
The occurrence dataset presented here can also be found at Deep-sea OBIS node https://doi.org/10.15468/szdxtb via GBIF.org
This shrimp could belong to the genus Benthesicymus (Benthesicymidae) or perhaps a shrimp of the family Aristeidae. It has a short rostrum with teeth and elongate pleopods. The image shows possible white corneas, seen previously amongst the Benthesicymidae. It is not possible to tell if the shrimp in the photograph has true white eyes or the white colour is a reflection from the strobe light. Fig.
In-situ images of Eumunida subsolanus described in
This crustacean looks much like J. californiensis (
Munidopsis sp. indet. 1 (Fig. 15), Munidopsis sp. indet. 2 (Fig. 16), Munidopsis sp. indet. 3 (Fig. 17) and Munidopsis sp. indet. 4 (Fig. 18). These images were taken at too great a distance to see fine details of the antennae, spines of the anterior carapace or other distinguishing features. However, all can be determined to belong to different species by the shape of the chelae, the colour and the length of the pereopods. Fig.
Munidopsis sp. indet. 1 (Fig. 15), Munidopsis sp. indet. 2 (Fig. 16), Munidopsis sp. indet. 3 (Fig. 17) and Munidopsis sp. indet. 4 (Fig. 18). These images were taken at too great a distance to see fine details of the antennae, spines of the anterior carapace or other distinguishing features. However, all can be determined to belong to different species by the shape of the chelae, the colour and the length of the pereopods. Fig.
Munidopsis sp. indet. 1 (Fig. 15), Munidopsis sp. indet. 2 (Fig. 16), Munidopsis sp. indet. 3 (Fig. 17) and Munidopsis sp. indet. 4 (Fig. 18). These images were taken at too great a distance to see fine details of the antennae, spines of the anterior carapace or other distinguishing features. However, all can be determined to belong to different species by the shape of the chelae, the colour and the length of the pereopods. Fig.
Munidopsis sp. indet. 1 (Fig. 15), Munidopsis sp. indet. 2 (Fig. 16), Munidopsis sp. indet. 3 (Fig. 17) and Munidopsis sp. indet. 4 (Fig. 18). These images were taken at too great a distance to see fine details of the antennae, spines of the anterior carapace or other distinguishing features. However, all can be determined to belong to different species by the shape of the chelae, the colour and the length of the pereopods. Fig.
Appears to be a goneplacoid crab. The overall habitus, aspects of the shape and colouration of the claws and shape of the carapace all fit well with Mathildellidae, based on the author's (S.Ahyong) extensive examination of many species of this group. Fig.
This could be Bathypalaemonella delsolari (
Reported from Peru (Sample NA064-022-01-01-A). Genetics could not provide idenfication beyond genus. The images were taken too far away to see features of the teeth on the rostrum or the relative length of the rostrum to the carapace and so neither Fig. 27 nor Fig. 28 can be identified beyond Nematocarcinus. Furthermore, it cannot be determined whether they are the same species or not. Species of Nematocarcinus have elongate, thread-like legs, barely visible in Fig.
The elongate, thread-like legs of this shrimp are easy to see in this photograph. However, as previously stated, the images were taken too far away to see features of the teeth on the rostrum or the relative length of the rostrum to the carapace and so neither Fig. 27 nor Fig. 28 can be identified beyond Nematocarcinus. Furthermore, it cannot be determined whether they are the same species or not. Fig.
Here we provide the first and most complete image inventory of arthropods found in the deep waters of the GMR to date. Of particular interest was the presence of three species that are new records to the GMR; Sternostylus defensus, Tylaspis anomala and Paromola rathbunae sp. inc. (Figs
The species of Eumunida subsolanus (Fig.
Overall, we observed many different types of arthropod behaviour and associations. For example, we found species from the genera Heteroptychus, Uroptychus, Eumunida and Sternostylus displaying a preference for gorgonians and black corals as hosts (Figs
We also recorded two rarely-observed deep-water hermit crabs Probeebei mirabilis and Tylaspis anomala (Figs
The brachyuran crab Paromola rathbunae sp. inc. was found carrying a sponge using its fifth pereiopods (Fig.
The polychelid lobster, Pentacheles laevis (Fig.
Since the 1950s, fisheries have been shifting towards deeper waters in most parts of the world, threatening deep-sea biodiversity and resulting in over-exploitation of seamount faunas (
This research was conducted under research permits PC-26-15 & PC-45-15 from the Galapagos National Park Directorate. The Seamounts of the GMR Research Project started in 2015 supported by a grant from the Helmsley Charitable Trust. This deep-sea exploration project was led by the Charles Darwin Research Station in collaboration with the Galapagos National Park Directorate, Ocean Exploration Trust and Rhode Island University. We thank the Government of Ecuador, via the Ecuadorian Navy and its Oceanographic Institute (INOCAR) for their support and permission to operate in their territorial waters. We would like to acknowledge the following people for their participation and contribution to this project: Etienne Rastoin, Elena Perez, Samuel Fischer, Belén Yanez and Patricia Marti-Puig. This publication is contribution number 2347 of the Charles Darwin Foundation for the Galapagos Islands.