Seafloor video-acoustic monitoring in a Greenlandic glacial fjord information hyperbenthos, backward-swimming fish, and narwhals

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Introduction

Arctic glacial fjords are hotspots of marine life, however they’re understudied because of their remoteness and troublesome entry, notably their seafloor ecosystems. Direct observations close to the seafloor can reveal biodiversity and animal conduct and are promising as a result of nearly all marine ecosystems studied thus far present a rise in biomass within the hyperbenthon (i.e., the benthic boundary layer) relative to the water mass instantly above it [1]. They are additionally doubtlessly useful in decoding different oblique measurements, resembling these obtained with lively acoustic profilers and hydrophones, which can’t confirm the sources of reflections or sounds [2]. However, it’s unclear if generally used monitoring strategies are noninvasive and appropriate, notably as a result of each lively and passive acoustic units are recognized to draw megafauna [3,4].

As a part of a long-term environmental analysis program since 2012 [5] and an acoustic monitoring program since 2019 [6] at Inglefield Bredning, northwest Greenland, a video digital camera with pink lights and a hydrophone had been deployed on the seafloor (260 m water depth) for about one week. This experimental strategy differs from different commercially accessible units that might be utilized in long-term mooring techniques or for hyperbentic sampling [1]. First, it doesn’t deter or entice animals with sound or gentle, as autonomous platforms with echo-sounders would possibly presumably do [3]. Second and third, in distinction to the excessive precision Underwater Vision Profiler, UVP [7], or submersible digital holographic cameras, like LISST-Holo2 [8], it information sound and permits monitoring objects bigger than macro-zooplankton (i.e., a couple of centimeters). Finally, it doesn’t pattern animals with backside sledges or traps [1].

Against this background, the target of this research was to doc the seafloor setting, assess its biodiversity, and consider the efficiency of a compact mooring system, together with its potential bodily interplay with narwhals (Monodon monoceros), which has just lately been recognized as a priority [4]. In specific, we hypothesize {that a} setup considerably shorter than beforehand used within the space and outfitted solely with passive instrumentation (together with acoustic and lightweight emitters) may be helpful for modern ecological research, whereas being much less invasive and fewer engaging to narwhals and different animals.

Materials and strategies

Study web site, setup, and information

The setup included an underwater digital camera synchronized to a hydrophone (LoggCAM; Biologging Solutions), a separate sound recorder (SoundTrap ST600, S/N 6229; Ocean Instruments), an acoustic launch (Ascent AR; Vemco), a buoy (Viny, 10B-8 with 10.7 kg of buoyancy; Kihoozai-kenkyuujo), an anchor (50 kg of rocks in a web), and a Samson 3/8” line connecting all parts into a sequence that’s ∼2.5 m lengthy (Fig 1). The mooring, excluding the anchor, matches right into a Zarges field, weighs lower than 15 kg, and is rated to 500 m water depth. The setup was first examined in a pool and shallow waters in Japan [9]. On 1 August 2025 (19:56 UTC), the setup was deployed in Inglefield Bredning, Greenland, roughly between Qeqertaq and Heilprin Glacier, from a ship to a water depth of ∼260 m (drop location: 77°28.120’N, 66°21.411’W). In this paper, all occasions are given in UTC (native time = UTC-1 h). This location was chosen as a result of it has the best chance of narwhal acoustic presence as in contrast with different monitoring websites inside the fjord [4]. On 9 August 2025 (15:31), the mooring was recovered utilizing a floor deck field VR100–300 with a transponding hydrophone VHTx-69kHz (Vemco) for distant opening of the acoustic launch. The work was performed beneath a Collaborative Research Agreement with the Greenland Institute of Natural Resources in Nuuk, with entry to the sphere web site permitted by the Danish Immigration Service.

During the interval of deployment, the digital camera was wanting upward and recorded 10-minute-long movies (VGA; 640×480 pixels at 30 frames per second) with audio (96 okayHz) each 20 min (i.e., with a 10-min pause between recordings) for about three days. The rationale for the upward viewing route, as in contrast with a downward route that might allow seafloor observations with out the buildup of sediment on the lens, was to movie narwhals, that are recognized to strategy from above and hit seafloor moorings [4]. Two LED lights on the digital camera had a pink wavelength (∼660 nm). This selection was made in an effort to keep away from overlap with the retinal absorbance of cetacean eyes [12] and for the presumably passive nature of the observations (i.e., in distinction to plain lights; e.g., [3,13,14]). However, because of the excessive absorbance of the pink wavelength, this selection restricted the vary of observations to <25–100 cm (Fig 1). The SoundTrap was outfitted with a strain reduction valve for deep water (Dual Seal PRV Ti – 20 psi; PREVCO Subsea), and constantly recorded sound at a sampling charge of 96 okayHz. The inner sensors of the acoustic launch recorded the temperature (±0.1°C decision), strain (±1 m decision), common noise, and tilt at 1-min intervals. In abstract, seven totally different streams of information had been collected [1517]. To interpret the water strain measurements and move variations, the information had been in contrast with sea-level information from Thule Air Base (renamed Pituffic station), that are collected each minute.

Data processing

A visible and aural evaluation of all video information was undertaken to detect and establish animals (on a 32-inch Retina 6K Pro Display XDR by Apple), primarily based on earlier research [1821]. Due to comparatively low picture high quality, attributable to pink lights and video decision, taxonomic identification was restricted to excessive taxonomic ranges.

Image and audio processing had been additionally undertaken. Existing Matlab features had been used to extract primary video-frame properties (https://www.mathworks.com/matlabcentral/answers/uploaded_files/74194/ExtractMovieFrames.m). Specifically, for each body, the whole space of the picture lined by particles was estimated, the variety of particles was counted, and the imply depth of the colour in every picture was computed.

Firstly, the background was faraway from every processed body to focus solely on shifting particles; i.e., by excluding any static, slowly various options, such because the extremely reflective PRV of the SoundTrap backside, the mooring line, with particles and fibers completely sticking to it (Fig 1), or sediments on the lens.

Secondly, the background was subtracted from every body, and the end result was binarized. This effectively highlighted the reflective particles and was then used to rely the variety of particles and combine their whole space. The whole space of every body lined by particles, A, is proven as a fraction of the whole picture measurement (i.e., A/[640 × 480]).

Thirdly, the body colour was handled as follows. True colour picture information had been specified for every pixel of the picture as a three-dimensional array of red-green-blue (RGB) triplets. The latter corresponds to a three-element vector, which specifies the intensities of the RGB parts of the colour as an integer of kind “unit8” from [0 0 0] to [255 255 255]. By computing the imply worth of every dimension for every body, the imply depth of the colour was extracted. During the descent of the digital camera via the water column, every RGB part was computed, and solely the temporal variation of pink on the seafloor because of the absorption of different colours was thought-about.

PIVlab was used to review particle movement within the movies (https://www.pivlab.de/). PIVlab is an open-source instrument for digital particle picture velocimetry (DPIV), which is a standard method in fluid dynamics and is also referred to as optical move evaluation [22]. To cut back the computational value, 10 frames had been analyzed from every file (0.3 s) as a substitute of processing full movies (150 Gb), and the end result vectors had been averaged for the dominant move magnitude and route. Based on the outcomes of the visible evaluation (S1 Table), a MATLAB GUI (https://github.com/GoldbergLab/manualObjectTracker) was used to manually monitor copepods within the movies (the one animals that repeatedly interacted with the setup).

Finally, each the digital camera and SoundTrap recorder had hydrophones recording on the identical sampling charge. However, as a result of the digital camera had 10-minute pauses and recorded just for three days, whereas the SoundTrap was sampling constantly and for the total period of the experiment, solely the SoundTrap acoustic information had been visualized, utilizing a long-term spectrogram (https://github.com/schonkopf/long-term-spectrogram).

Results

Overview

The key variables measured throughout the digital camera deployment are proven in Fig 2. The water depth oscillated round 260 m with the tide (amplitudes as much as 1.5 m). Measurements began on the minimal tidal vary (neap tide), and ended earlier than the utmost tidal vary (spring tide); consequently, the digital camera observations corresponded to the weakest tidal circumstances. The imply temperature of the water was −0.18°C. The tilt of the discharge was fixed (3.6°), according to the movies that confirmed no movement or vibration of the setup. The imply background noise degree was 169 mV, with spikes akin to narwhal ultrasonic vocalizations which are seen on the spectrogram of the SoundTrap information. Narwhals had been acoustically current day-after-day, besides 6 August 2025 (noticed as elevated ultrasound power at >20 okayHz; Fig 2). At decrease frequencies, the first geophonic supply was the rumbling, cracking, and melting of icebergs (<10 okayHz). Boat engine noise was additionally recorded (<5 Hz).

Camera

Animals

By manually reviewing all 223 video information (37 h in whole), we recognized actively swimming Amphipoda, heteropods (Pterotracheoidea), arrowworms (Chaetognatha) and bristle worms (Polychaeta), abruptly leaping Copepoda, jellyfish (Hydrozoa), comb jelly (Ctenophora), fish, shrimp (swimming Decapoda), Mysida, and different not recognized animals (Fig 3; S1 Table; S1 Video). The organisms had been by no means noticed in teams, and normally floated individually, aside from some amphipod pairs. In addition, none of those organisms was related to concurrently recorded sounds, aside from a shrimp scratching the digital camera and a narwhal. Narwhals had been the primary supply of biophonic sounds, though they didn’t work together with the mooring and appeared in digital camera view solely as soon as, on 5 August (05:23:13), when high-amplitude narwhal sounds co-occurred with the sluggish movement of a tusk tip within the background, which was tens of centimeters from the buoy (S1 Video).

The whole variety of detected specimens was 478 (differentiated in no less than 11 taxa), akin to roughly 1 detection each 5 minutes. The detection frequency for every class of animal is proven in Fig 4. Amphipoda had the best prevalence (47%), adopted by Copepoda (26%), Hydrozoa (8%), and Chaetognatha (8%; with just one bristle worm, Polychaeta). The remaining ∼12% of detections had been primarily unidentified organisms and in addition fish, Decapoda, heteropods, and Ctenophora. The detection occasions for probably the most considerable organisms didn’t present any clear sample (Fig 4).

The copepods are presumed to be Calanoida on account of their comparatively giant measurement. Specifically, within the frames of some movies (e.g., Nos. 2, 95, and 106), Copepoda collided with the mooring line, for which we all know the diameter, indicating antennulae (the primary antennae, A1) lengths of as much as a centimeter. Interestingly, on the time of collision, the copepods jumped away from the mooring line whereas drawing their antennulae alongside their physique sides. Such jumpy propulsion was additionally noticed with none apparent contact with the setup (Fig 5).

The extremely lively arrowworms, which present attribute undulatory locomotion [23], had been almost certainly Eukrohnia hamata. Clearly filmed fish had been a Liparidae (additionally known as snailfish within the literature [24]). One snailfish confirmed peculiar backward swimming, passively drifting backward with the present (Fig 5). It curled its tail and remained immobile for no less than 16 s earlier than disappearing from view. The shrimps had been probably Decapoda Thoridae. Both Liparidae and Decapoda Thoridae are recognized to be narwhal prey within the fjord [25].

Suspended matter

At the seafloor, the video revealed quite a few small particles and hair-like fibers of various measurement, which we confer with as “marine snow” and assum to be of natural or blended origin. Dense fiber clouds had been additionally noticed, spinning in entrance of the digital camera. These had been typically attributable to organisms, resembling fish or shrimp passing close by (S2 Video). In normal, marine snow was continually shifting throughout the scene. Within a single video file (10 min lengthy), the route, quantity, and velocity of movement of particles diverse considerably. Usually, the movement was translational (i.e., with particles shifting horizontally previous the digital camera). However, often, vertical and vortical movement was additionally evident when particles precipitated, advected away from the lens, or confirmed obvious shear, with nearer and farther particles shifting in reverse instructions.

Automatically extracted options are introduced in Figs 78. The proportion of every picture lined by particles and absolutely the variety of particles diverse considerably with time (Fig 7A,B). The imply proportion of every picture lined by particles was 0.95±0.8% (STD), whereas the imply variety of particles was 85±22 (STD). The depth of pink gentle in every picture (Fig 7C) was managed by the reflecting particles, with three forms of transient anomalies ensuing from the brightness spike of the primary body (i.e., taken instantly after turning the digital camera on), animals attaching to the lens, and sediment that had collected quickly on the lens (Fig 7DE). Power spectral density evaluation didn’t reveal clear cyclicity within the temporal variation of the extracted options (S1 Fig).

While the motion route and velocity of particular person particles between two sequential frames might be extremely variable, the averaged information confirmed clear 12 h oscillations in these variables (Fig 8; S3 Video). A comparability with the tidal information means that the route of particle movement reverses at excessive and low water (presumably round slack water). The Pearson’s linear correlation coefficient, r, between the sea-level change and the angle of particle movement was 0.54 (p-value = 4 × 10−14). Moreover, particles moved on the highest speeds throughout the durations with quicker change in water degree (Fig 8; r = 0.57; p-value = 2 × 10−16). This highlights the position of tidal currents in particle transport close to the seafloor. Given that the rising tide brings water into the fjord, this suggests that the higher edge of every picture faces the inside components of the fjord and the decrease edge faces oceanward.

Discussion

During the three days of digital camera observations, there have been no bodily interactions between giant objects (resembling narwhals) and the mooring, regardless of their each day acoustic presence. It is unclear whether or not this mirrored the quick period of the experiment or the specified lack of curiosity in regards to the mooring system that was ten occasions shorter than beforehand used [4]. The extent of narwhal sensitivity to pink gentle from the digital camera (660 nm) stays unsure, given the problem of conducting such experiments and the dearth of experimental validation. However, it’s unlikely that the narwhals had been deterred by the digital camera lights, as a result of retinal pigments of different deep-diving odontocetes are usually not delicate to such wavelength [12,26], and their sensitivity is shifted in the direction of blue gentle, equally to mesopelagic-dwelling fish [27].

No aggregations of fish or different animals had been noticed across the mooring. As such, the mooring was not a refuge, and thus was unlikely to have been a foraging attractor for narwhals [4]. The apparently weak aggregation impact is attention-grabbing, as a result of fish-aggregating units, FADs, are generally used to feed fish and shelter (https://www.fisheries.noaa.gov/national/bycatch/fishing-gear-fish-aggregating-devices). The FADs are floating units on the floor, and it’s potential that floating objects are much less efficient at shut vary to the underside. We acknowledge that the quick deployment interval could have led to this end result.

Most of the noticed animals might be recognized due to earlier regionally related publications [1821], and abdomen content material evaluation by the authors [25,28]. The explored group corresponded to the hyperbenthos, a time period referring to the affiliation of small animals inhabiting the water layer adjoining to the seafloor [1]. As there is no such thing as a literature on the hyperbenthos within the research space, and low taxonomic decision just isn’t conducive to detailed comparability with different areas, we restrict our temporary dialogue to normal factors, useful relationships, and sampling methodology. Amphipods, copepods, medusae, chaetognaths, and decapods are typical residents of the hyperbenthos. Mysida, nonetheless, thought-about a serious part of this group and used to detect degradation in response to chemical contaminants [29], was noticed solely as soon as. Many fish and crustaceans prey on the hyperbenthos and have a hyperbentic life type at formative years phases [1]. Commonly, these communities are sampled utilizing backside sledges and nets, implying that our research offers an alternate methodological strategy which may be much less dependable for taxonomic identification however yields insights into extremely cellular animals of their pure setting.

The excessive detection charge of Amphipoda and their comparatively speedy swimming behaviour close to the seafloor is according to their scavenging position underwater [4]. The escape response of copepods (Fig 5) has beforehand been studied within the laboratory utilizing high-speed cameras [30], however such direct visible observations of free-swimming copepods in deep waters are uncommon. The escape response seems to primarily characterize predator-avoidance conduct triggered by the mechanical sensitivity of the primary antennae. Light is an unlikely set off, as many copepods drifted via the sunshine cone with none response.

Liparidae are vertebrates finest tailored to depth and the deepest recognized fish (down to eight,145 m; [13]). In distinction to the backward swimming by reverse undulation noticed for different deep-sea fishes [14], one Liparidae drifted with the present within the current research (Fig 5). Similar conduct has been reported for Liparidae off the coast of central California [24]. Given that this fish doesn’t have a gasoline bladder, it’s not anticipated to be detectable by lively acoustic units [2].

Subglacial meltwater discharge types near-surface plumes in entrance of glaciers which are foraging hot-spots for birds and seals, because of the entrainment of deep water in the direction of the floor [31]. In the current research, the deployment was not made precisely on the calving entrance of the glacier; nonetheless, the deployment depth and destructive water temperatures are just like these on the foot of the beforehand studied Bowdoin Glacier, which can also be situated in Inglefield Bredning Fjord [31,32]. Therefore, contemplating the exceptionally robust upwelling (which is steady in summer time) and a excessive chance of an osmotic shock [31], it’s affordable to recommend that the species recognized within the movies may be carried upward by subglacial plumes and develop into simple prey. For instance, abdomen content material evaluation has revealed that Amphipoda, Liparidae, and Decapoda are preyed upon by seals within the space, whereas Copepoda are probably prey for sea-birds and ringed seals [28]. Copepoda are the one class that may enter the hyperbenthos from above and return to the water column each day. Due to insufficiently exact taxonomic decision, it stays unclear whether or not copepods, amphipods, and shrimps within the hyperbenthos characterize totally different species from these within the stomachs and the water column. However, throughout the open-water interval, 4 ringed seals tagged with satellite-relay information loggers spent most of their time within the neighborhood of tidewater glacier fronts at depths shallower than 100 m [33], additional suggesting that they could profit from foraging alternatives close to the floor.

The DPIV revealed tide-modulated adjustments in move velocity and route over time, in addition to turbulent vortices, highlighting the extremely lively seafloor circumstances (Fig 8). Moreover, an in depth video evaluation indicated that some particle vortices (and thus water mixing) had been produced by passing animals (S2 Video, S3 Video), which may additional obscure or masks the dynamics at bigger scales. There was no clear diurnal or semidiurnal pattern within the different extracted parameters (e.g., the variety of particles and animals; Figs 4, 6, and S1 Fig), presumably because of the small quantity of monitored water, quick period of the video information (3 days), and weak tidal part throughout the commentary interval. This quick period and an absence of observations throughout spring tide circumstances temporally restrict conclusions about each day vertical migrations and tidal results. Nevertheless, provided that the clear tidal modulation of particle movement was detected throughout neap tide circumstances, it’s affordable to recommend that spring tide observations would possibly yield a stronger modulation of the thought-about parameters.

For areas with a excessive charge of sedimentation, resembling close to glaciers or rivers [32], the upward orientation of the digital camera may be disadvantageous and result in a completely obscured lens. In such circumstances, a downward-looking setup may be extra appropriate, though the photographs may be saturated in extraordinarily turbid waters.

A guide evaluation of video information is a really time-consuming. To detect an organism, their swim patterns had been as vital as their form. Going forwards and backwards between the frames whereas discussing the goal with as much as three co-authors skilled in species identification required roughly twice as a lot time because the video period itself, and corresponded to no less than 74 working hours. In this research, a guide evaluation was wanted to label and understanding the information. However, in future, a machine imaginative and prescient workflow ought to be explored for processing giant information units. The labeled dataset may be helpful as coaching information for such a function (S1 Table).

Due to the excessive red-light absorbance and low picture decision, the digital camera had a restricted discipline of view. On the one hand, our reliance on pink gentle may correspond to a decrease chance of interference with animal conduct (e.g., Copepoda react to regular gentle [30]). On the opposite hand, this would possibly cut back the detection likelihood and introduce bias. Moreover, poor visibility would possibly lead to passively flowing creatures being ignored or misidentified as particles. For instance, in some movies (0141*.mov; > 05:42), the amphipod ceased motion and continued to move with the present. Furthermore, the quite a few fibers may be jellyfish tentacles. This means that some organisms might be missed, particularly throughout high-speed move. Therefore, it’s applicable to deal with the reported organism counts as detections somewhat than as abundance estimates. This may be remedied by the next video decision.

Conclusion

Overall, the examples introduced above spotlight the potential of our strategy for modern environmental and organic research on the seafloor. So far, there have been few direct underwater observations within the Arctic for ecological analysis. With video setups changing into accessible [34], extra research can be useful for filling this data hole. At this stage, the short-term setup of the current research, which inserts into one Zarges field, is appropriate for speedy deployments and comparative research in numerous areas.

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