1. Introduction
Understanding the processes that influence a species distribution and its dynamics is particularly relevant for conservation [
1]. This information may assist in mapping biodiversity and ecosystem services, identifying effects and potential threats of environmental changes and anthropogenic activities, enabling effective prioritization of areas for biodiversity conservation. It also provides crucial knowledge to develop tools and models used in conservation [
1,
2]. To obtain a comprehensive view of these processes, it is mandatory to understand the life history traits and the biology of the species as well as the environmental factors to which the species may respond. Marine species that are capable of large-scale movements have a high dispersal potential especially in continuous environment like open ocean where physical barriers are not obvious [
3,
4]. Yet, several studies showed high residency and site fidelity patterns in marine species where movements were influenced by environmental barriers and biological factors such as mating success, access to breeding grounds or access to consistent food resources. For instance, reef fishes show limited connectivity between reefs separated by large sand channels [
5,
6], killer whales display intrinsic isolation of communities due to different food resources [
7], bottlenose dolphins demonstrate restricted home range linked with productive habitats [
8] and oceanic whitetip sharks record high site fidelity driven by the consistent availability of prey [
9]. Food resource is also a major factor that influence the movement of large-bodied filter-feeding species [10-12]. Yet, this resource depends on environmental factors resulting in different distribution patterns between regions of the world. Consequently, spatial distribution and dynamics of these highly mobile filter-feeding species may be different from one region to the next.
Reef manta rays (
Mobula alfredi, (Krefft, 1868)) are filter-feeders found in tropical waters around the word. Populations are observed near coastal reefs and their movements have been documented to be driven by the availability of food resources. For instance, in the Maldives, seasonal peaks in productivity gather hundreds of individuals each year [
13]. In Indonesia, reef manta rays perform long distance migration triggered by monsoon shifts and associated reduction in productivity [
14]. In Australia, highly productive eddy events are likely to trigger offshore movements of individuals [
15] and seasonal variations in temperature appears to initiate latitudinal migration over hundreds of kilometres along the east coast of Australia [
16,
17]. In contrast, when the resource is consistent throughout the year, reef manta rays seem to demonstrate strong residency patterns with only few connections between geographically close populations. In Hawaii, no connection was found over 10 years of photo-identification monitoring between two aggregation sites located only 150 km apart. Similarly, in Indonesia, acoustic telemetry suggested spatial segregation between populations that are only 150 km apart [
18]. These evidences suggest that the spatial ecology of reef manta rays can be difficult to predict and that localised investigation might be necessary to obtain comprehensive understanding of their movements. This is a crucial task as the species is heavily exploited in many regions of the world for their gill plates that are used in Asian medicinal trade [
19]. In addition to this fishing pressure, reef manta rays exhibit several conservative life history traits that exacerbate this vulnerability including small population size, low fecundity and fragmented distribution. Their strong affinity for coastal shallow waters increases their exposition to human activities, such as bycatch fisheries [
20], uncontrolled mass tourism [
21,
22], habitat degradation [23-26], boat strikes [
27] and fish nets entanglement [
28]. Consequently, reef manta rays are classified vulnerable to extinction on the IUCN Red List of Threatened Species [
29]. Providing robust information on the movement patterns and habitat use of reef manta rays would contribute to the design of effective management and conservation measures that are essential to protect the species.
Among methods that enable spatial analysis, satellite telemetry is now a common practice with an increasing number of studies deploying tags to track movements of a wide range of species including terrestrial species, marine birds, sea turtles, marine mammals, and elasmobranchs [2,30-37]. This tool allows researchers to investigate broad-scale and fine scale movements, diving behaviour as well as preferred depth and temperature, and sometimes revealing misconceptions or unexpected findings about the ecology of a species [38-40]. Satellite tracking devices are effective tools to detect unsuspected large migrations in elasmobranchs such as the basking shark [
41], the six gills shark [
42] and the white shark [
43], for example.
In New Caledonia, reef manta rays have not been studied until recently [
46,
47,
48] and basic information on the population of this emblematic and threatened species are needed. Previous findings using four years of photo-identification monitoring revealed that the population of reef manta rays was distributed in all parts of the archipelago and exhibited high long-term fidelity rates at these sites. Connectivity was also limited but possible between all sites showing high dispersal potential [
47]. In addition, genomic analyses found genetic differentiation between aggregation sites, which confirms the importance of site fidelity and exacerbated the lack of connectivity between geographically close habitats [
48].
On this basis, we use satellite tracking to investigate the spatial ecology of M. alfredi in the fragmented environment of the New Caledonia archipelago. Our objectives are to assess the fine scale habitat use and potential broad scale migration patterns by addressing the following points: quantify the use of offshore versus coastal waters, show the extend and limitation of the movements from aggregation sites with high fidelity rates, define the frequency and magnitude of the connectivity between studied sites, detect potential broad scale movements and the existence of unknown key habitats.
4. Discussion
In New Caledonia, reef manta rays tend to remain close to coasts and reefs. Except for one individual, all records were within 35 km off the closest reef. Several studies that documented movements of reef manta rays reported consistent use of coastal and reef areas in Australia [
15,
54], in the Red Sea [
55,
56], in the Seychelles [
57], and in the British Indian Ocean Territory MPA [
58]. The use of coastal habitat by reef manta rays and other planktivorous elasmobranchs has been associated with food availability [13,24,59-63]. Coastal areas of islands surrounded by deep waters are prone to assemble the conditions to generate primary productivity hotspots combining upwellings and land inputs and generating reliable food resources which might result in strong residency pattern in reef manta rays’ behaviour [
57,
64]. In New Caledonia, such conditions exist with little annual variations [
65,
66]. Limited offshore movements are likely due to the foraging ground being coastal and the probable lower productivity of the adjacent oceanic waters [
67]. Other than food resources, coastal areas and shallow waters of the lagoon offer more protection from predators such as large sharks and hence, represent a suitable environment for potential nurseries. In New Caledonia, the detection of juvenile individuals remains sporadic, and neonates are even scarcer, although lagoons are places of nursery grounds for reef manta rays in Raja Ampat, Indonesia [
64] and for other elasmobranchs [68-70]. Further investigations in suspected adequate nursery grounds using aerial surveys and accurate measurement methods to quantify maturation stages might lead to the discovery of nurseries in New Caledonia. In addition, coral reefs are also home to numerous cleaning stations that are essential to manta rays’ well-being and health [
71], as well as mating and socialization [
72,
73]. Sheltered waters also act as a thermal refuge where enclosed shallow waters have a significantly higher temperature than oceanic waters. In this study, manta rays were observed to favour relatively high temperatures (27 to 29 °C) but were also able to face much colder water for instance when deep diving (7.6 °C). Basking in warm shallow waters after a deep dive would allow regulation of the body temperature. Thermoregulation is an important part of the behaviour of mobulids [
45,
74] and other elasmobranchs [
75,
76] and the presence of warm-sheltered water in proximity of deep feeding grounds might be essential.
The use of offshore waters by one individual recorded in this study could be interpreted as a transiting trip toward potential alternative foraging grounds near isolated reefs. Presence of reef manta rays at isolated reefs have already been recorded during aerial surveys [
77], further investigation in these areas might reveal new aggregations. Offshore movements by reef manta rays were also documented using satellite telemetry and were associated with foraging opportunities. In the east coast of Australia, [
15] recorded most of the tagged rays in the offshore Capricorn Eddy Region and attributed this behaviour to be food related to the high productivity generated by the eddy. In the Red Sea, [
55] observed offshore excursions to deeper water at night where manta rays performed deep dives supposedly to exploit pelagic planktonic resources.
Despite their demonstrated coastal affinity, reef manta rays have been observed over waters up to 2,720 m deep. The archipelago of New Caledonia has a relatively narrow continental shelf, especially on the east coast of the Main Island and around the Loyalty Islands, beyond which water depth drops rapidly. Even though manta rays spent most of their time within the first 50 meters, our results suggest that this species is able to use deeper water to transit between areas (e.g.; to connect with an isolated reef) or to access to demersal food resources [
78]. This supports previous findings that recorded reef manta rays commuting between islands chain separated by deep water in Indonesia [
14,
64] or transiting by deep water to access food resources in east Australia [
15] and the Maldives [
79]. However, even if there are evidence that deep water is not a strict barrier to their movements, large expanses of deep water might still be a restricting factor to connectivity. For instance, in this study, spatial occupancy overlapped only for individuals originating from sites sharing the same coastline and not for individuals separated by a 2,000-meter-deep channel. Other evidence through different spatial and temporal scale using photo-identification [
47] and genomics [
48] showed that these connections occur but were limited, highlighting the lack of connectivity over this deep-water channel. Other studies taking place in atolls were consistent with these observations with populations recording no or only few connections between islands separated by deep waters in Hawaii [
80,
81], in the Maldives [
82], in French Polynesia [
83] or in the Seychelles [
57]. On the contrary, reef manta rays showed long distance movements along continuous coastlines, up to 1150 km in east Australia [
84], but also along the west coast of Australia (up to 700 km, [
54]) or the coast of southern Mozambique (up to 350 km, [
85]).
Horizontal movements were classified into four distinct patterns. The most dominant pattern was
Fidelity where manta rays remained within their home range for the whole duration of the tag deployment. Manta rays displayed also excursions travelling, occasionally, relatively long distance as far as 131 km away from the site of origin. Moreover, total track lengths were relatively small (maximum of 688 km) in comparison to previous findings averaging 839 km in western Australia [
54], 1169 km in east Australia [
15] and 1074 km in the Seychelles [
57]. Our results describe a behaviour that corresponds to site fidelity as defined by Chapman et al. (2015): the return of an individual to a location where it previously resided after an absence as long as or longer than the residency period [
86]. Additional evidence of such behaviour was found in New Caledonia using long-term photo-identification data to find high re-sighting rates for each site [
47] and genomics analysis to detect genetic structure between sites [
48]. Site fidelity is often motivated by consistent foraging opportunities over time within an area [
86]. This behaviour has been largely documented for reef manta rays in Hawaii [
81], Mozambique [
87], east Australia [
60], Indonesia [
64,
88] or French Polynesia [
83]. Although most of the tagged individuals displayed constrained movements near the aggregation site of origin, manta rays of New Caledonia demonstrate the ability to potentially connect with all parts of the archipelago, at least parts that are linked by coastlines or shallow waters. In particular, almost a third of the individuals showed
Relocation and
Fidelity + Relocation patterns, connecting with sites up to 311 km from the site of origin. Coupled with return trips over 200 km away from the deployment location, these observations suggest that manta rays connect to intermediate sites. For instance, while no connection was observed between studied sites during this study, overlap occurred for individuals from Touho and Noumea at in-between sites along the east coast and at the southern tip of the Main Island. Sightings of manta rays using photo-identifications over five years revealed different aggregation sites throughout the archipelago with multiple re-sightings from individuals originating from different sites [
47]. The present results suggest the potential existence of additional aggregation sites where manta rays from different sites may encounter each other, although no field operation could be undertaken to confirm it.
The present results present a partial short-term overview of the spatial ecology of the reef manta rays of New Caledonia. The average deployment duration in this study was short (approx. 77 days) compared to what was achieved in other satellite telemetry studies on reef manta rays (e.g.; 92 days, [
15]; 147 days, [
55]; 116 days, [
57]). This might also explain the relatively smaller track lengths recorded in this study than at other locations in the world. To complement this finding, long term monitoring of the movements and geographically extended sampling effort might help deciding whether these observations are sporadic, frequent, seasonal or to what extend long-term site fidelity is supported. They may as well reveal new connections and new potential aggregation sites. To this regard, photo-identification offers such perspectives and acoustic telemetry may narrow the gap between photo-identification and satellite telemetry by generating spatially and temporally intermediate data. In addition, genomics would provide a greater picture of the evolutionary processes that shape the population.
5. conclusions
This work used satellite telemetry and confirmed that reef manta rays are resident to coastal water and show strong site fidelity in New Caledonia. Yet, this species is capable of relatively long-distance migrations seemingly favouring, but not limiting them to, coastal and shallow water paths. Deep water might be a restraining factor but not a complete barrier to connectivity. These results raise concerns regarding threats associated with habitat degradation, human exploitation and disturbance. The home range of this species may also extend over greater distances than previously thought, especially in habitat fragmented by deep waters, which raises concerns regarding potential movements outside areas under protective jurisdictions. In New Caledonia, concerns regarding the species conservation are limited since reef manta rays are not targeted by fisheries and human activity remains relatively low. Such favourable context is scarce which makes the population of reef manta rays in New Caledonia a reference to be preserved [
19]. Therefore, preventive precautions should be taken at local level where coastal development is rapidly expanding and might threaten critical habitats.