- Marine Record
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Southern elephant seal vagrants in Ecuador: a symptom of La Niña events?
Marine Biodiversity Recordsvolume 11, Article number: 13 (2018)
Extralimital observations of pinnipeds are important to understand the effects of changing climates on our oceans and the distribution of these species. The southern elephant seal (Mirounga leonina) is a known vagrant species that moves over long distances. We report three new records of M. leonina in interior freshwater tributaries of the Guayas River Estuary Basin (Gulf of Guayaquil) and northern coast of Ecuador between October 2017 and January 2018 during a cold episode of La Nina event in the southeastern Pacific.
The elephant seals were identified according to their large size (~ 5 m for adult and 2–3 m for juveniles/subadults), the head to neck size ratio, and the size and external morphology of the proboscis, which was used as a key trait to differentiate M. leonina from the Northern elephant seal (M. angustirostris). The observations of M. leonina in Ecuador highlight an extreme movement covering an assumed total distance of approximately 8000 km from the circumpolar region. The cold event “La Niña” with sea surface temperature anomalies ranging − 1.5 °C to − 0.5 °C in October 2017 likely triggered the extralimital movements of these animals.
Recurring observations of M. leonina in the Guayaquil Gulf suggest the importance of this highly productive region and tropical estuarine-riverine habitats as temporary haulout sites for resting. These new findings indicate that vagrant individuals influenced by oceanographic events and eco-physiological processes are reaching this region more frequently than previously thought.
The southern elephant seal (Mirounga leonina) is the largest pinniped in the world and is not habitually found in tropical areas because of its circumpolar and sub-Antarctic distribution in the southern ocean (Le Boeuf and Laws 1994; Jefferson et al. 2015). Adult southern elephant seals present a marked sexual dimorphism due to their polygynous system (Le Boeuf 1974; Baldi et al. 1996). Adult males can be much larger than females and have a long proboscis; males reach a length of up to 5–6 m and a maximum weight of 4000 kg, while females measure ~ 3 m and weigh 400–900 kg (Le Boeuf and Laws 1994; Modig 1996; Jefferson et al. 2015). The global southern elephant seal population has been estimated at 700,000 individuals greater than one year of age, with an annual production of 189,000 pups (Le Boeuf and Laws 1994; Lewis and Campagna 2005; McMahon et al. 2005).
This species is widely distributed in the circumpolar and sub-Antarctic islands, where it is assembled in three population groups: South Georgia, Kerguelen and Macquarie (Deméré et al. 2003; McMahon et al. 2005). The South Georgia population group is comprised of the populations existing on the South American continent, including the Valdés Peninsula and Malvinas Islands (Slade et al. 1998; Hoelzel et al. 2001), as well as a small colony located in Ainsworth Bay, Magallanes Region (i.e. XII Region of Magallanes) and Chilean Antarctica (Vargas 2012). Breeding and moulting haulouts, as well as winter haulouts of southern elephant seals are also found at Marion Islands, South Africa (Kirkman et al. 2001; Kirkman et al. 2003; Kirkman et al. 2004).
The life cycle of M. leonina has two terrestrial stages, including a stage dedicated to moulting (predominantly from December to February) and another for reproduction (September–October). This species has two ocean life stages, i.e. post-moulting and post-reproduction (Campagna et al. 1993; Le Boeuf and Laws 1994). During the non-breeding season, adult and sub-adult males tend to undertake large migrations over thousands of kilometers in the Antarctic Ocean for feeding, with some vagrant individuals observed beyond or outside of their normal range (Hindell and McMahon 2000; Fabiani et al. 2003; Lewis and Campagna 2005; Lewis et al. 2006; Campagna et al. 2006; Reisinger and Bester 2010; Jefferson et al. 2015).
Oceanographic-atmospheric events such as El Niño (i.e. ENSO events) and La Niña have severe impacts affecting the migration patterns and feeding trips of pinnipeds (Alava and Salazar 2006; Avila et al. 2015; Alava and Aurioles-Gamboa 2017; Elorriaga-Verplancken et al. 2016, Páez-Rosas et al. 2017; Quintana-Rizzo et al. 2017). These changes are generally associated with the availability of food due to the displacement of prey towards colder regions or deeper waters (Soto et al. 2004; Trites et al. 2007). For instance, La Niña is accompanied by a decrease in sea surface temperature (SST), producing changes in ocean circulation dynamics around the South American continent and eastern Tropical Pacific (Kessler 2006). This event can lead to anomalies in the distributional pattern of tropical species, or in the migration of species from relatively cold waters to warmer areas (Ballance et al. 2006).
The dispersal capacity of pinnipeds has contributed to the movement of several species (e.g., harbour seals, Phoca vitulina; hooded seal, Cystophora cristata; southern elephants seals, M. leonina, Juan Fernandez fur seal, Arctocephalus philippii; Galapagos fur seals; Arctocephalus galapagoensis; Guadalupe fur seals, Arctocephalus towsendi) hundreds or even thousands of kilometers away from their feeding or breeding areas (Johnson 1990; Reeves et al. 2002; Alava and Carvajal 2005; Avila et al. 2015; Alava and Aurioles-Gamboa 2017; Páez-Rosas et al. 2017; Quintana-Rizzo et al. 2017), with many sightings involving cases associated with vagrant adult individuals at sea and along coastal regions during their feeding trips. Southern elephant seal adults have been reported resting on the coasts of Brazil, Ecuador, Galapagos Islands, Chile, Panama, Peru, South Africa, Australia and New Zealand (Reeves et al. 2002; Magalhães et al. 2003; Vargas and Steinfurth 2004; Lewis and Campagna 2005; Alava and Carvajal 2005; Lewis et al. 2006; Sepúlveda et al. 2007; Acevedo et al. 2016; Mayorga et al. 2017; Stewart and Felix 2018). Of particular relevance here is the presence of southern elephant seals reported in 1998 and 2002 in the Gulf of Guayaquil, Ecuador (Alava and Carvajal 2005), where the authors suspected both animals to be vagrant M. leonina and photos of the animals suggest this identification is reliable (Alava and Carvajal 2005; Jefferson et al. 2015).
In this work, we report apparently healthy M. leonina in the Guayas River Basin (Gulf of Guayaquil) and on Ecuador’s north coast, and discuss the possible influence of La Niña event as a driving atmospheric-oceanographic force affecting the distribution and behavioral patterns of the species.
Four sightings of elephant seals in the Gulf of Guayaquil and on the coast of Ecuador between October 2017 and January 2018 are described here. The first record is located at the Babahoyo River sub-basin, which is one of the main tributaries of the Guayas River, in the Gulf of Guayaquil (Fig. 1). The Guayas River is formed at the confluence of the Babahoyo and Daule Rivers. The elephant seal was first sighted on 24 October 2017 in apparently healthy condition (i.e. signs of emaciation and external injuries were not observed) and hauling out on the riverbanks of the Milagro River (2°6′33″ S, 79°41′10″ W), a small river located at the Yaguachi Municipality (Guayas Province) approximately 75 km from the outer estuary of the Guayaquil Gulf at the Ecuadorian Pacific (Fig. 1). The elephant seal was photographed (Fig. 2a), and monitored by the Wildlife Department (Ministry of Environment of Ecuador) for a period of 24 h. Subsequently, the Civil Defense and Firefighter departments arrived at the site to prevent harassment from the local people and allow the elephant seal to move from this river and enter the Babahoyo River.
Following this event, an elephant seal was spotted on 28 October 2017 and assumed to be the same individual due to the similar size and infrequent occurrence of this species in the region (Fig. 2b). The animal was swimming farther north of the Milagro River along the Arenal River (1°46′22″ S, 79°39′58″ W). The Arenal River is a small inland river from the Municipality of Baba (Los Ríos Province) flowing into the Babahoyo River, and located at approximately 105 km from the outer estuary of the Guayaquil Gulf. After these two sightings, the animal was no longer recorded in the region, suggesting that the elephant seal left the coast and continued with its feeding trip in the Pacific Ocean.
Succeeding these sightings, two other reports of elephant seals were made along the Ecuadorian coast. A second individual (Fig. 2c) was observed on 10 December 2017. This animal was spotted for about two hours hauling out around an inland freshwater flooded and mud-covered field and the riverbanks of a narrow creek at the Yaguachi Municipality, Guayas Province (2°5'48.5'' S, 79°41'41.4'' W). The third animal was recorded in the northern coast of Ecuador at Tonsupa, Esmeraldas Province (0°53'12" S, 79°48'46" W), on 24 January 2018. This individual was resting on the beach, where it was exhibiting signs of moulting (Fig. 2d). Apparently, the same animal was spotted ten days later further south in Atacames, Esmeraldas Province (0°52′ N, 79°50′ W) on 3 February 2018 by personnel from the Ministry of Environment of Ecuador, who monitored the animal and corroborated that was the same individual observed in Tonsupa (R. Carvajal, pers. comm., 5 February 2018).
The taxonomic identification of the sighted animals was based on the external morphological attributes, including body size and coloration, ratio of neck to head size, and the shape and size of the proboscis, following guides of marine mammal species identification (e.g., Reeves et al. 1992; Reeves et al. 2002; Jefferson et al. 2015).
Given the morphological similarity between the southern elephant seal and its congener species the northern elephant seal (M. angustirostris), we performed a photographic review comparing and contrasting images of these two species. This includes photos of the large males described in this work (Figs. 2a, b, and 3a), a photo of an adult male of M. angustirostris from San Benito Islands, Mexico (Fig. 3b; taken by the first author, Dr. D. Paéz-Rosas) and photos of a subadult and adult male M. leonina from the Valdez Peninsula, Argentina (Fig. 3c and d; courtesy of Dr. M. Drago). Since in previous sightings of elephant seals in 1998 and 2002 in the Gulf of Guayaquil (Alava and Carvajal 2005), it was not possible to describe the species with exact morphological details, the photographic records of these two individuals were also revisited.
Furthermore, the possible influence on the displacement of elephant seals towards tropical waters in Ecuador in the Eastern Pacific by negative anomalies in SST was examined. Then, the link to La Niña events, which are associated with cold conditions and primary productivity increase in the southeastern Pacific Ocean, was also assessed. Monthly anomalies of SST time series data were calculated with respect to historical climatological values (i.e. 1971–2000) in this region; SST values were obtained from the NOAA website (http://www.emc.ncep.noaa.gov/research/cmb/sst_analysis/).
The pinniped observed on October 24–28 was identified as an adult male M. leonina. Based on our observations and the analysis of Figs. 2a-b and 3a, this individual might correspond to a specimen of a total length of 4–5 m and weight of 2000 kg. Conversely, the individuals sighted on December 10 and January 24 were identified as immature or subadult animals, resembling a ~ 2 m-length young male (Fig. 2c), and a subadult male of ~ 4 m of length (Fig. 2d), respectively.
From the photographic review of images of southern elephant seals and northern elephant seals, a taxonomic identification of these animals was achieved. The major distinctive, external morphological trait to differentiate the two species in males is the proboscis, which is shorter and smaller in M. leonina (Figs. 2a and 3a) compared to the proboscis of M. angustirostris, shown in Fig. 3b (Jefferson et al. 2015; Dr. L. Huckstadt, pers. comm.; Dr. F. Elorriaga-Verplancken, pers. comm., October 2017). While both species possess an enlarged nose, the proboscis in M. leonina hangs down in front of the mouth (Fig. 3a, c and d), while the proboscis in M. angustirostris is significantly longer, and can extend 15–25 cm below the lower lip (Jefferson et al. 2015). Likewise, in adult males, the neck is bulkier in relation to the head (i.e. the head to neck size ratio) in M. leonina (Fig. 3a, d) compared to that of M. angustirostris (Fig. 3b).
As for the juvenile M. leonina, the individual depicted in the Fig. 2c showed similar features to the elephant seals observed in both 1998 and 2002 in the Gulf of Guayaquil (see Fig. 1 in Alava and Carvajal 2005). Comparably, the subadult male observed at Tonsupa (Fig. 2d), showed similar features to the subadult elephant seals of the Valdez Peninsula (Fig. 3c). Both individuals (Fig. 2c, d) had undeveloped proboscises and good body conditions. Following the sighting of the animal recorded in Tonsupa, a subadult M. leonina was observed shortly after at Pianguita beach (3°52′38″N, 77°1′36″W; Buenaventura, Valle del Cauca, Colombia), in late January 2018 and in the Choco region (Dr. I. Avila, pers. comm., January and April 2018).
Based on monthly anomalies of SST time series data calculated with respect to historical climatological values from 1971 to 2000 in the southeastern Pacific region, the presence of La Niña event was confirmed during October 2017, as illustrated in Fig. 4. These negative temperature anomalies (i.e. -1.5 °C to − 0.5 °C) and cold conditions are directly related to an increase in primary productivity levels around the area of incidence of the Humboldt Current (Ballance et al. 2006; Wang and Fiedler 2006). Therefore, we believe that the displacement of these individual seals towards tropical waters in Ecuador can be associated to a cooling La Niña event registered in the region.
Discussion and conclusions
Vagrant individuals of M. leonina have been reported to reach the central coast of Chile and Juan Fernandez Islands, Ecuador (Gulf of Guayaquil), Brazil’s coast, southern Africa, southern Australian coast, Tasmania and New Zealand, as well as the coast of Oman (Arabian Peninsula), and the Island of Taboga (Gulf of Panama), which was the northernmost record thus far reported (Lodi and Siciliano 1989; Johnson 1990; Reeves et al. 2002; Magalhães et al. 2003; Alava and Carvajal 2005; Sepúlveda et al. 2007; Jefferson et al. 2015; Acevedo et al. 2016; Mayorga et al. 2017; Stewart and Felix 2018).
While the moulting and non-breeding seasons are critical stages obliging elephant seals to disperse to different feeding grounds, and, temporarily, haul out on land as part of their annual cycle during December–February (Campagna et al. 1993; Le Boeuf and Laws 1994), epidermal moult (i.e. sloughing and shedding of patches of fur with skin attached) was apparently observed in the subadult sighted (Fig. 2d) at Tonsupa (Esmeraldas) on January 2018, but not in the individuals recorded in October or December 2017, nor in the elephant seals recorded in December 1998 and February 2002 (Alava and Carvajal 2005). Thus, moulting cannot be considered thus far as the only physiological factor influencing the arrival of elephant seals on Ecuador’s coast.
The ecological implications of these new extralimital records are important and illustrate the possible influence of climatic-oceanographic variations on the migratory patterns of M. leonina. In fact, the adult male reported here is assumed to have dispersed over a geographic range of ~ 8000 km from the circumpolar/sub-Antarctic region in the Southern Ocean to tropical freshwater systems in the Gulf of Guayaquil, Ecuador. Because of the good body condition (i.e. emaciation or dehydration was not observed) of the observed adult male and juveniles, and the similarity in the sighting locations where subadult individuals were reported in 1998 and 2002 (during periods when the La Niña event also took place (Alava and Carvajal 2005), this work highlights the importance of La Niña as a driving environmental/natural force influencing the distribution and migratory behavior of this species.
This cold event is likely to have influenced or stimulated these elephant seals to pursue the cool, nutrient rich mass of water along the South American Pacific coast (Fig. 4), and thus extending their foraging trip outside the established geographic range, possibly explaining their arrival to the rivers of the Ecuadorian coast as previously proposed (Alava and Carvajal 2005). Top predators from Southern Ocean and Antarctic, including pinnipeds (i.e. southern elephant seals, M. leonina, crabeater seals, Lobodon carcinophaga, and Weddell seals, Leptonychotes weddelli) from a changing Southern Ocean and Antarctic, forage in regions where physical climatic forcing and specific oceanographic features are responsible for enhanced and increased availability of prey (Costa et al. 2010). In this context, we further postulate that the presence of sub-Antarctic pinnipeds such as southern elephant seals outside their habitual feeding or reproduction grounds would be associated with cooling periods such as La Niña.
These observations emphasize the need to strengthen collaboration and cooperation with other research groups not only at the local or regional level, but along the Pacific coast of South America and Antarctica with the aim to develop and maintain a monitoring and research program. These monitoring approaches can include satellite tracking and telemetry deployed in pinnipeds to be used as oceanographic sentinels to understand oceanographic data and key features of the southeastern Pacific, where traditional scientific oceanographic cruise and shipboard platform are limited or absent (Costa et al. 2010). This initiative will also help to assess and track distributional and behavioral patterns of pinnipeds throughout South America, mainly when there are years with anomalous oceanographic conditions that may affect the distribution, regional movements and migration of vagrant species.
El Niño Southern Oscillation
Sea surface temperature
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We thank the Ministry of the Environment of Ecuador for providing us with the information about the sightings and the state of the animal. Finally, we thank Dr. Leonardo Zurita and MSc. Daniela Alarcón-Ruales for help in the preparation of Fig. 1, as well as Dr. Fernando Elorriaga-Verplancken, Dr. Luis Huckstadt, Dr. Massimiliano Drago and Dr. Isabel Ávila for their valuable advice for the identification of the species, the facilitation of the photographs and comments during the planning of this manuscript. We are indebt with Dr. Victoria Otton for proof reading and providing edits and insights to improve this manuscript.
The University of British Columbia (UBC, Canada), the Universidad San Francisco de Quito (USFQ-Ecuador) and Fundación Ecuatoriana para el Estudio de Mamíferos Marinos (FEMM) provided logistical and financial support during the planning and preparation of this work.
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