- Open Access
Simple criteria to determine detachment point of towed satellite tags provide first evidence of return migrations of whale sharks (Rhincodon typus) at the Galapagos Islands, Ecuador
© Hearn et al.; licensee BioMed Central Ltd. 2013
- Received: 22 March 2013
- Accepted: 3 July 2013
- Published: 6 August 2013
Attachment of towed, floating satellite tags to large marine organisms has provided scientists with a wealth of information on the movements of these species. These tags generally are not programmed to detach at a particular time, yet are often prone to detachment by natural means after only a few days or weeks. It is important to be able to distinguish between the tracks provided by a detached, floating tag, and one that is attached to the subject. To this end, we placed three SPOT-5 and one SPLASH tag on large female whale sharks at Darwin Island (Galapagos Islands), and compared their tracks with those of two floating SPOT-5 tags released at the same site. We present a set of criteria to determine whether a towed satellite tag encased in a float is still attached to the study organism.
None of the whale sharks remained in the vicinity of the island. Three of the tracks lasted 31 to 48 days, yet one shark was tracked for 167 days. This was the first recorded bona fide homing migration of a whale shark, travelling 1,650 km west then returning to Darwin four months later. Two other sharks also returned to Darwin. We found that at the time of detachment, a clear change in the daily timing and quality of transmissions became evident. This, in conjunction with daily depth and temperature summaries, and knowledge of currents and the biology of the subject, can be used to justify endpoints on tracks that continue to accrue positions as the tag floats with the currents.
The data provided by floating tags is sufficiently distinct to be able to determine a detachment date. After detachment, daily transmissions are received in the first hours of the day after midnight (Coordinated Universal Time), the location quality of the transmissions is consistently high, and temperature or depth summaries are consistent with surface records. Prior knowledge of subject behavior and general ocean circulation patterns in the region reinforces the ability to determine detachment date. In some cases, after a prolonged period of more than three or four weeks, the detection pattern may change, yet caution should be exercised in assuming that the tag is, after all, still attached.
- Galapagos Islands
- SPLASH tag
- SPOT tag
- Tag detachment
- Whale shark
The use of satellite transmitters (or tags) to track the movements of large marine organisms across the oceans has become a common tool across a range of disciplines over the last two decades (see reviews; [1–3]). These tags commonly use the Argos low polar orbit satellite system , which uses the Doppler effect on transmission frequency to estimate positions, when the tag is at the surface and a satellite is overhead. For large, free-swimming species, it is often appropriate to place the tag in a torpedo-shaped float, and attach it to the subject by means of a dart and a tether of varying length. Eventually, the tag is likely shed, and may spend an indeterminate period floating at the surface, transmitting data to the satellite system. It is important to be able to distinguish between a tag that is attached to the subject and one that has detached and is floating. This issue has rarely been addressed in the literature (although see ) and may lead to debatable tracks - the longest recorded track of a whale shark, travelling 13,000 km from the Gulf of California across the Pacific , has been questioned recently  due to the distance of around 10,000 km between the main portion of the track and the last few data points. In addition, floating tags may in some cases provide us with some information about the behavior of the focal species. For example, a floating tag was used to show by comparison the highly oriented movements made by scalloped hammerhead sharks, Sphyrna lewini, at seamounts in Baja California, Mexico .
Smart positioning tags (also known as SPOT tags) are programmed to transmit near-real-time positions when the study organisms are at the surface. They may also transmit limited temperature information, in the form of the percent time spent at user-specified temperature bins. A variation of these, known as SPLASH tags, also provide similar summaries of time at depth. SPOT and SPLASH tags come in several forms, depending on the focal species. The towed, floating arrangement has been used to track basking sharks, Cetorhinus maximus, off the British Isles ; to describe the movements of whale sharks, Rhincodon typus, in the Gulf of California ; to compare the movements of tarpon, Megalops atlanticus, with their bull shark, Carcharhinus leucas, predators in southern Florida ; and manta rays, Manta birostris, to determine their association with seasonal oceanographic features off the Yucatan Peninsula, Mexico . Yet the greatest number of individuals tagged and tracked over the widest geographic range are whale sharks .
Whale sharks are the world’s largest fish, reaching maximum reported lengths of 20 m , and are known to spend significant periods of time at or close to the surface [12, 13]. They therefore make a good model species for the exploration of tag detachment issues. Predictable seasonal aggregations of whale sharks, often related to feeding, have been reported at certain locations, including Ningaloo Reef, Western Australia; Gladden Spit, Belize; Baja California, Mexico; Holbox Island off the Yucatan Peninsula, Mexico; and the Maldives [14–16]. All these aggregations are made up predominantly of males, and most individuals were below 10 m in length [7, 17–19]. Whale sharks are known to move large distances  and their movements or presence at some sites have been linked with oceanographic features [20, 21]. However, true migration, implying the movement away from a location over a long distance and a subsequent return, has not been registered to date , although photo identification studies have shown that individuals persist at sites over extended periods .
Here, we present tracks from an ongoing study to determine the movement patterns of mostly large, female whale sharks that occur seasonally at the Galapagos Islands, Ecuador . By comparison with data from tags deployed directly into the water, we explore how the timing and quality of the transmissions, the depth and temperature data, and the tracks themselves can help us to determine whether and when a tag has detached from the subject organism.
Summary of whale shark tracks
8 July 20111
8 September 2011
5 September 2012
6 September 2012
Estimated total length (m)
Track length (days)
Estimated detachment date
1. Transmission times
24 December 2011
16 October 2011
7 October 2012
25 October 2012
2. Transmission qualities
24 December 2011
15 October 2011
6 October 2012
23 October 2012
15 October 2011
6 October 2012
13 October 2012
24 December 2011
15 October 2011
6 October 2012
23 October 2012
The 10 m female (WS-2) initially moved 100 km to the northeast, but returned to within 30 km of Darwin a week after the tag was attached. The tag detached about 300 km to the east of Darwin, although the cumulative distance travelled by the shark during the track was 1,044 km.
The smallest whale shark (WS-3, 5.9 m) provided a 31-day track of a single directed movement to the southwest for a distance of approximately 1,725 km, at which point the tag detached. Its overall movement rate was around 55 km/d (0.65 m/s).
The largest whale shark (WS-4, 11 m) made repeated northeast-southeast movements, reaching a maximum distance of 620 km southeast of Darwin, on 3 October 2012, three weeks after tagging (moving a cumulative distance of 1,830 km at an overall rate of 67 km/d). It then returned almost directly to Darwin over a period of a week at a much faster overall rate of 98 km/d, and was detected within 50 km of the island on 12 and 13 October 2012, after which it began to move west.
The two floating tags (FL-1 and FL-2) drifted westwards to the open ocean with the South Equatorial Current for approximately 1,200 km, then circled northwards into a eddy at about 4°N and 100°W (Figure 2). However, FL-1 reached the eddy in two weeks, traveling at an average speed of 78 km/d (or 0.9 m/s), whereas FL-2 took two months to cover the same distance, at an average speed of 20.8 km/d (or 0.25 m/s).
The tracks presented in this study suggest that whale sharks do not reside at Darwin, but rather that Darwin is a common location in their long-distance movements. With the exception of southern Baja California , Darwin is the only location where large, apparently gravid females make up most of the observed population. All three of the sexually mature, apparently pregnant females returned to within 75 km of Darwin several weeks after tagging, and, although in all cases the track continued elsewhere, these make up the first published tracks of return movements. The only whale shark not to make a return movement was the immature female.
The track for WS-1 ended along the shelf break of northern Peru, corroborating the presence of whale sharks in Peru, where they have previously only been recorded anecdotally .
Our results show that, by using a combination of transmission times and qualities along with temperature or depth summaries, it is usually possible to determine when detachment occurred. We would expect to see a consistent pattern of daily transmissions beginning at midnight (UTC) and ending only a few hours later when the programmed daily allowance of transmissions has been reached. Similarly, we would expect the location quality to be higher from a floating tag than from one subjected to drag from a moving subject below the surface. The antenna would be submerged more often, and hence the salt water switch would turn off the signal transmission. If there is information on general ocean circulation patterns in the area, this also facilitates the process. Little support for passive diffusion by currents as a factor influencing whale shark distribution was found in the north eastern Indian Ocean, with swimming speeds up to three times greater than the maximum surface current velocities that whale sharks encountered .
We propose that future studies using towed satellite tags make explicit reference to the criteria used to determine detachment points. We chose to rank our criteria in order of simplicity, such that the first step is the creation of a simple scatterplot of detection times per day, obtained from the raw Argos log. When all transmissions occur during the first few hours after midnight each day for a prolonged period, this is a clear indication of a detached tag. Second, there is a break in the daily quality of locations with a greater proportion of high quality positions occurring when the tag has detached. Third, where depth data are not available, temperature histograms used in conjunction with sea surface temperature data from the study area can be used to show that the detached tag is permanently in the top layer of the water column. Finally, if the track follows the prevailing current, this may be used to validate the assumption that the tag has detached.
In most cases, all detachment criteria will coincide (Table 1). Our sample size was small (only two floater tags and four tags deployed on whale sharks), and in other instances there may be confounding effects of more variable currents and rough seas preventing floating tags from transmitting in such a regular fashion. However, this provides a rapid means of flagging potential detached tags without the need for any additional data besides the raw Argos logs.
When all the criteria do not coincide, such as with WS-4, it may be necessary to use prior knowledge of the subject species to make a judgment call. For example, we determined that it was unlikely a whale shark would remain at the surface constantly for a month, based on previously published information on whale shark diving behavior [12, 13]. Rather, we assume that the tag detached and floated for a month, then become entangled with another organism. However, given the ambiguity in this case, we might consider presenting the entire track, but displaying where there is uncertainty so that readers can to come to their own conclusion.
The increasing literature on whale shark movement patterns provides us with more data for justifying track endpoints. For example, based on published information on diving behavior for whale sharks, the longest recorded track of a whale shark, travelling 13,000 km from the Gulf of California across the Pacific , has recently been questioned  due to the distance of around 10,000 km between the main portion of the track and the last few data points. Again, given what we can glean from the existing sample size of tagged whale sharks, it is unlikely that it would have travelled that distance over that time period without spending sufficient time at the surface for the satellites to pick up a transmission.
Whale sharks utilize Darwin’s Arch for brief periods during large scale movements in the Eastern Tropical Pacific. All three of the mature, apparently pregnant females briefly returned close to Darwin (within 75 km) after absences of one week to three months, before continuing their movements. The longest track (almost five months) ended off the shelf break of northern Peru. Darwin Island appears to serve as a waypoint for pregnant females on a larger scale migration between the coast of South American and the open ocean.
The data provided by floating tags is sufficiently distinct to be able to determine a detachment date. After detachment, daily transmissions are received in the hours following midnight (UTC), the location quality of the transmissions is consistently high, and temperature or depth summaries are consistent with surface records. Prior knowledge of subject behavior and local current patterns reinforces the ability to determine detachment date. In some cases, after a prolonged period of more than three or four weeks, the detection pattern may change, yet caution should be exercised in assuming that the tag is, after all, still attached. A period of rough seas might disturb this pattern briefly, and the tag becomes fouled or entangled over time. We suggest that where there is uncertainty about the nature of the track, this should be made explicit.
Whale sharks were tagged off Darwin Island, Galapagos at a location known as Darwin’s Arch (1.6725°, -91.989°). At this site, a rocky platform at a depth of approximately 7 m drops almost vertically to over 30 m along a 300 m stretch. Although whale sharks may be sighted infrequently throughout the Galapagos Archipelago, Darwin’s Arch has become an important site for dive tourism, partly due to the predictable occurrence of small numbers of whale sharks from June through November each year (coinciding with the cool season). Our research cruises were timed to coincide with the start, middle and end of the whale shark season. Tags were deployed in different months in 2011 (WS-1 on 8 July, WS-2 on 8 September, FL-1 on 14 July, FL-2 on 1 September) and in 2012 (WS-3 on 5 September, WS-4 on 6 September).
Our search strategy consisted of two dive teams, each made up of a photographer, a tagger and a support diver. Both teams patrolled Darwin’s Arch at the drop off, awaiting the arrival of whale sharks. Whale shark encounters ranged from none to five for each 40-minute dive. Due to strong currents and dive depth limitations, not every encounter resulted in a tagging attempt. We attached the tags to the sharks via 1.5 m tethers made from stainless steel cable and stainless steel darts. Tags were coated with a non-metal based antifouling paint prior to attachment. The tags were attached to the shark in front of or immediately behind the base of the first dorsal fin by use of a pneumatic spear gun. The total length of the sharks was estimated using laser photogrammetry , whereby a photo of the flank of the whale shark was taken using a camera with two laser pointers at a known distance apart (in this case, 50 cm) and then the length between the fifth gill and first dorsal fin was scaled up to the total length of the shark (r2 = 0.93) . The gender of sharks was evident by the presence or absence of claspers as observed by the dive team in situ and, where possible, confirmed with photographic or video evidence.
All interactions with whale sharks were carried out in accordance with the University of California Davis Animal Care Protocol #16022.
We used five position-determining satellite tags (SPOT-5; Wildlife Computers, Redmond, WA, USA), on both floating tags and the three pregnant females. We used one depth-recording tag (SPLASH; Wildlife Computers) on the immature female. The tags are encased in torpedo-shaped floating housings. They are unable to transmit while underwater, but are fitted with a wet-dry sensor that determines when they are on the surface, at which time they begin to transmit to Argos satellites. The positions of the tags are determined by Doppler shift in transmissions received by the satellite, and assigned a quality depending on the associated error of the position and the number of messages per pass. In cases where at least four messages are received, the quality class is numerical: 3 (error of the position <250 m), 2 (error of the position 250 to 500 m), 1 (error of the position 500 to 1,500 m), 0 (error of the position >1500 m. Where fewer than four messages are received, there is no error estimate and the quality is assigned a letter: A (three messages), B (one or two messages) . The tags were programmed to transmit a maximum of 300 times a day, with no carryover to the next day if the allowance was not completed.
The SPLASH tag provided 12-hour summaries of depth, in the form of the percentage time spent at pre-programmed depth bins (ranging from 0 to <1200 m), while the SPOT-5 tags provided similar summaries for time spent at different temperatures (see axes on Figure 6 for individual tag settings). For both tag types, the summaries were timed to coincide with local dawn and dusk.
For each tag, we created a scatter plot of transmission times for each day and a histogram of the quality of transmissions each day. The amount of time spent per day at different depth (SPLASH tag) and temperature (SPOT-5 tags) was also plotted for each tag, using DeltaGraph software (Red Rock Software, Inc., Salt Lake City, UT, USA).
We filtered the position locations obtained from the Argos system to remove duplicate messages, and to remove positions that implied sustained movements greater than 2 m/s. We used the remaining positions to create tracks using ArcMap 9.0 (ESRI, Redlands, CA, USA).
We obtained information from general ocean circulation patterns for the area from the literature . At Darwin Island, the prevailing current is the South Equatorial Current, which flows to the west. To the north of this is the North Equatorial Countercurrent, which flows in the reverse direction.
The whale shark research project for the Galapagos Islands was funded by the Blake, Kimberly and George Rapier Charitable Trust, by grants issued through Conservation International and The Galapagos Conservancy. Thanks to the Captain and Crew of the Queen Mabel. We wish to acknowledge the in-field support of Yasmania Llerena, Inti Keith, Gabriel Vazquez, Jules Paredes and Pelayo Salinas. The fieldwork was carried out under permits PC-37-11 and MAE-PNG/CDS-2012-0020 from the Galapagos National Park Service.
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