Um total de 142 crânios do boto-de-Burmeister, Phocoena spinipinnis depositados em museus e coleções cientificas da Argentina, Brasil, Chile, Peru e Uruguai foram utilizados para explorar a variação geográfica em relação ao tamanho e forma do crânio de P. spinipinnis. Ademais, foi realizada uma caracterização oceanográfica da área de distribuição do boto-de- Burmeister através de dados históricos de temperatura, salinidade e oxigênio a 0 e 50m de profundidade na costa Atlântica e Pacifica. As idades dos animais foram obtidas pelas leituras das GLGs na dentina. A idade mais alta atingida por ambos os sexos foi de 10 anos. Medições na dentina mostraram dimorfismo sexual na primeira GLG e diferenças geográficas entre botos do Peru e Atlântico. Três tipos de anomalias foram registrados nos dentes, e a linha marcadora parece estar associada ao “El Niño”. Vinte e oito caracteres métricos foram utilizados para explorar o dimorfismo sexual e crescimento. A maturidade física do crânio foi estabelecida quando o comprimento côndilo-basal atingiu 95% do comprimento total (≥266mm nos machos e ≥277mm nas fêmeas). Diferenças no tamanho e forma do crânio foram analisadas através de morfometria tradicional e geométrica. Os resultados revelaram dimorfismo sexual, sendo as fêmeas maiores do que os machos. As diferenças em tamanho e forma concentraram-se principalmente na região rostral e neurocrânio. Foi observada variação geográfica entre os botos do Atlântico, Chile e Peru. P. spinipinnis do Peru são de menor tamanho em relação a os botos do Chile e Atlântico. Botos do Chile apresentam um tamanho e forma intermediária, e os botos do Atlântico são maiores (especialmente na região orbital, altura do crânio e região rostral). A distância de Mahalanobis mostrou maior separação entre os botos do Peru e do Atlântico, e menor distância entre os exemplares do Chile e Atlântico. A morfometria geométrica explica com maior clareza as diferenças entre botos do Chile e Atlântico, especialmente nas vista ventral e lateral. A correlação entre variáveis ambientais e morfométricas através da análise de correlações canônicas e dos quadrados mínimos parciais de dois blocos sugere que as diferenças observadas no tamanho e na forma dos crânios têm uma importante influência espacial, associada à variabilidade sazonal das condições oceanográficas presentes nos dois oceanos e diretamente relacionada às três áreas oceanográfica propostas neste estudo: (1) de Paita, Peru (05°01’S, 81ºW) até o sul do Golfo de Arauco, Chile (∼39°S); (2) do sul do Golfo de Arauco até o sul do Rio da Prata (∼38°S); e (3) do Rio da Prata até Santa Catarina, Brasil (28º48’S; 49°12W). Adicionalmente, propõe-se que P. spinipinnis apresenta uma distribuição contínua desde Paita, Peru ate a bacia do Rio da Prata, Argentina, podendo alcançar águas uruguaias e brasileiras em determinadas condições oceanográficas (entrada de águas mais frias e menos salinas com direção ao norte, associadas à Convergência Subtropical) / A total of 142 skulls from Burmeister’s porpoises, Phocoena spinipinnis from museums and scientific collections from Argentina, Brazil, Chile, Peru and Uruguay were analyzed to explore the geographical variation in relation to size and shape on skulls of P. spinipinnis. In addition, an oceanographic characterization of the area of distribution of Burmeister’s porpoise by historical data of temperature, salinity and oxygen the 0 and 50m of depth on the Pacific and Atlantic coast was carried out. The age of the animals was obtained by reading the Growth Layer Group in dentine. The oldest male and female were 10 years of age. Measurements in dentine showed sexual dimorphism in the first GLG and geographic differences between porpoises from Peru and Atlantic. Three types of anomalies were recorded in teeth, and the marker lines seem to be associated to “El Niño”. Twenty-eight characters were used to explore sexual dimorphism and growth. Physical maturity of the skull was established when 95% of condylobasal length was attained (≥266mm in the males and ≥277mm in the females). Differences in size and shape of skull were analyzed by traditional and geometric morphometrics. The results revealed sexual dimorphism, being the females larger than male, and the differences in size and shape are concentrated mainly in the rostral region and neurocranium. Geographic variation between porpoises from Atlantic, Chile, and Peru was observed. P. spinipinnis from Peru are smaller compared to porpoises from Chile and Atlantic. Porpoises from Chile have an intermediate shape, and porpoises from Atlantic are larger (mainly related to orbital region, skull height and rostral region). The distance of Mahalanobis showed more separation between porpoises from Peru and Atlantic, and less distance between specimens from Chile and Atlantic. Geometric morphometrics was more useful for show differences between specimens from Chile and Atlantic, especially in the ventral and lateral views. The correlation between environmental and morphometric variables by canonical analysis and two-block partial least squares suggests that the differences observed in the size and shape of skulls would have an important spatial influence, associated to the seasonal variability of the oceanographic conditions present in the two oceans, and directly related to the three oceanographic areas proposed in this study: (1) from Paita, Peru (05°01’S, 81ºW) to south of Arauco Gulf, Chile (∼39°S); (2) from south of Arauco Gulf to south of La Plata River, Argentina (∼38°S); and (3) from La Plata River to Santa Catarina, Brazil (28º48’S; 49°12W). In addition, it is proposed that P. spinipinnis presents a continuous distribution from Paita, Peru to La Plata River basin, Argentina, being able to reach Uruguayan and Brazilian waters under certain oceanographic conditions (intrusion of colder and less saline waters toward the north associated with the Subtropical Convergence).

Um total de 142 crânios do boto-de-Burmeister, Phocoena spinipinnis depositados em museus e coleções cientificas da Argentina, Brasil, Chile, Peru e Uruguai foram utilizados para explorar a variação geográfica em relação ao tamanho e forma do crânio de P. spinipinnis. Ademais, foi realizada uma caracterização oceanográfica da área de distribuição do boto-de- Burmeister através de dados históricos de temperatura, salinidade e oxigênio a 0 e 50m de profundidade na costa Atlântica e Pacifica. As idades dos animais foram obtidas pelas leituras das GLGs na dentina. A idade mais alta atingida por ambos os sexos foi de 10 anos. Medições na dentina mostraram dimorfismo sexual na primeira GLG e diferenças geográficas entre botos do Peru e Atlântico. Três tipos de anomalias foram registrados nos dentes, e a linha marcadora parece estar associada ao “El Niño”. Vinte e oito caracteres métricos foram utilizados para explorar o dimorfismo sexual e crescimento. A maturidade física do crânio foi estabelecida quando o comprimento côndilo-basal atingiu 95% do comprimento total (≥266mm nos machos e ≥277mm nas fêmeas). Diferenças no tamanho e forma do crânio foram analisadas através de morfometria tradicional e geométrica. Os resultados revelaram dimorfismo sexual, sendo as fêmeas maiores do que os machos. As diferenças em tamanho e forma concentraram-se principalmente na região rostral e neurocrânio. Foi observada variação geográfica entre os botos do Atlântico, Chile e Peru. P. spinipinnis do Peru são de menor tamanho em relação a os botos do Chile e Atlântico. Botos do Chile apresentam um tamanho e forma intermediária, e os botos do Atlântico são maiores (especialmente na região orbital, altura do crânio e região rostral). A distância de Mahalanobis mostrou maior separação entre os botos do Peru e do Atlântico, e menor distância entre os exemplares do Chile e Atlântico. A morfometria geométrica explica com maior clareza as diferenças entre botos do Chile e Atlântico, especialmente nas vista ventral e lateral. A correlação entre variáveis ambientais e morfométricas através da análise de correlações canônicas e dos quadrados mínimos parciais de dois blocos sugere que as diferenças observadas no tamanho e na forma dos crânios têm uma importante influência espacial, associada à variabilidade sazonal das condições oceanográficas presentes nos dois oceanos e diretamente relacionada às três áreas oceanográfica propostas neste estudo: (1) de Paita, Peru (05°01’S, 81ºW) até o sul do Golfo de Arauco, Chile (∼39°S); (2) do sul do Golfo de Arauco até o sul do Rio da Prata (∼38°S); e (3) do Rio da Prata até Santa Catarina, Brasil (28º48’S; 49°12W). Adicionalmente, propõe-se que P. spinipinnis apresenta uma distribuição contínua desde Paita, Peru ate a bacia do Rio da Prata, Argentina, podendo alcançar águas uruguaias e brasileiras em determinadas condições oceanográficas (entrada de águas mais frias e menos salinas com direção ao norte, associadas à Convergência Subtropical) / A total of 142 skulls from Burmeister’s porpoises, Phocoena spinipinnis from museums and scientific collections from Argentina, Brazil, Chile, Peru and Uruguay were analyzed to explore the geographical variation in relation to size and shape on skulls of P. spinipinnis. In addition, an oceanographic characterization of the area of distribution of Burmeister’s porpoise by historical data of temperature, salinity and oxygen the 0 and 50m of depth on the Pacific and Atlantic coast was carried out. The age of the animals was obtained by reading the Growth Layer Group in dentine. The oldest male and female were 10 years of age. Measurements in dentine showed sexual dimorphism in the first GLG and geographic differences between porpoises from Peru and Atlantic. Three types of anomalies were recorded in teeth, and the marker lines seem to be associated to “El Niño”. Twenty-eight characters were used to explore sexual dimorphism and growth. Physical maturity of the skull was established when 95% of condylobasal length was attained (≥266mm in the males and ≥277mm in the females). Differences in size and shape of skull were analyzed by traditional and geometric morphometrics. The results revealed sexual dimorphism, being the females larger than male, and the differences in size and shape are concentrated mainly in the rostral region and neurocranium. Geographic variation between porpoises from Atlantic, Chile, and Peru was observed. P. spinipinnis from Peru are smaller compared to porpoises from Chile and Atlantic. Porpoises from Chile have an intermediate shape, and porpoises from Atlantic are larger (mainly related to orbital region, skull height and rostral region). The distance of Mahalanobis showed more separation between porpoises from Peru and Atlantic, and less distance between specimens from Chile and Atlantic. Geometric morphometrics was more useful for show differences between specimens from Chile and Atlantic, especially in the ventral and lateral views. The correlation between environmental and morphometric variables by canonical analysis and two-block partial least squares suggests that the differences observed in the size and shape of skulls would have an important spatial influence, associated to the seasonal variability of the oceanographic conditions present in the two oceans, and directly related to the three oceanographic areas proposed in this study: (1) from Paita, Peru (05°01’S, 81ºW) to south of Arauco Gulf, Chile (∼39°S); (2) from south of Arauco Gulf to south of La Plata River, Argentina (∼38°S); and (3) from La Plata River to Santa Catarina, Brazil (28º48’S; 49°12W). In addition, it is proposed that P. spinipinnis presents a continuous distribution from Paita, Peru to La Plata River basin, Argentina, being able to reach Uruguayan and Brazilian waters under certain oceanographic conditions (intrusion of colder and less saline waters toward the north associated with the Subtropical Convergence).

De part l'importance et la diversité des pressions anthropiques en mer du Nord, les mammifères marins en tant que prédateurs supérieurs se trouvent de plus en plus exposés à ces activités (trafic maritime, activités industrielles et portuaires, surpêche, pollution chimique, etc.). Les campagnes d'observation SCANS et SCANS II mises en place en 1994 et 2005 pour estimer l'abondance des petits cétacés, ont mis en évidence un changement majeur dans la distribution du marsouin commun (Phocoena phocoena) en mer du Nord avec un déplacement du Nord vers le Sud. Ce changement peut être lié à une migration de ses proies préférentielles en mer du Nord et/ou à une afaptation de son régime alimentaire par rapport à la disponibilité des proies. Parallèlement, à ces modifications de distribution spatiale, un nombre croissant d'échouage de marsouin commun en Manche Orientale et sur les côtes belges a été observé depuis une dizaine d'années avec une augmentation conséquente ces deux dernières années. Pour étudier les causes responsables de ces échouages, un des objectifs de cette étude a été d'évaluer l'état de la contamination chimique des animaux échoués en relation avec l'état sanitaire des individus. L'analyse de deux familles de composés chimiques (éléments traces métalliques et polluants organiques persistants) sur des animaux échoués sur la période 2006-2013 révèlent des concentrations significativement plus élevées dans les organies des animaux présentant des pathologies que celles obtenues chez les animaux sains. Cette tendance a déjà été observée en Atlantique Nord pour le marsouin. Les comparaisaons des niveaux de concentration mesurées avec ceux d'études antérieures effectuées sur des marsouins échoués dans la même zone ou dans le Golfe de Gascogne suggèrent que l'augmentation du nombre de marsouins échoués n'est pas liée à une dégradation du milieu en terme de pollution chimique. Pour déterminer le régime alimentaire du marsouin commun, trois techniques complémentaires ont été utilisées : l'analyse des contenus stomacaux, des isotopes stables (carbone et azote) et des acides gras dans différents tissus. Pour ces deux dernières méthodes, les signatures obtenues pour le marsouin ont été comparées à celles de leurs proies potentielles. Les résultats ont mis en évidence la présences des gobies, merlans, lançons, sprats, trisopterus sp., harengs et sardines comme proies potentielles. Le déplacement des marsouins du nord jusqu'au sud de la mer du Nord a été attribué à la baisse de l'abondance du lançon dans le nord, ainsi qu'à la ré-invasion du sud de la mer du Nord par la sardine, probablement suite au changement climatique. Enfin, cette étude confirme la nécessité d'utiliser une approche multi-analyses qui intègre des informations complémentaires à différentes échelles de temps pour étudier le régime alimentaire de ces prédateurs supérieurs. / The North Sea is heavely impacted by human activities such as overfishing and pollution. Due to their position as top predators in the ocean, marine mammals are becoming increasingly affected by anthropogenic activities. The large-scale surveys SCANS in 1994 and SCANS II in 2005 that were held in the North Sea to estimate the abundance of small cetaceans highlighted a major shift in the distribution of harbour porpoises (Phocoena phocoena) from the northern parts of the North Sea to its eastern parts. Alongside, over the past few decades harbour porpoises stranding has increased in the southern North Sea particularly along the French and Belgian coastal waters. Since the contaminant exposure presents, among others, a potential threat to harbour porpoises inhabiting the North Sea, the first objective of the present study was to assess the contamination status of this species in the southern North Sea. On the other hand, the distribution and abundance of marine mammals is expected to follow the distribution of their main prey species. Hence, the second objective of this study was to investigate whether the changes in the distribution of porpoises in the southern North Sea may be a result of the changes in prey availability. Moreover, the third objective was to evaluate the interest of combining three methods to investigate the diet of harbour porpoises : stomach contents, stable isotopes (carbon and nitrogen) and fatty acids analyses. First, the contamination status was evaluated through the determination of two components of chemical contaminants (metals and persistent organic pollutants) in tissues of harbour porpoises stranded along the southern North Sea between 2006 to 2013. Several chemical contaminants presented higher concentrations in diseased animals compared to healthy animals. In addition, some metallic contaminants showed bioaccumulation with age. Comparison with previous study suggests that the population status of harbor porpoises in term of chemical concentration has been stable from 1994 to 2013. This work suggested that the increase in the number of stranded individuals is not related to the decline in the quality of the environment. Secondly, the shift in the abundance of harbour porpoises was evaluated and interpreted in the light of prey species abundance. Three techniques were used in order to determine the diet of porpoises. Results highlighted the presence of gobies, whiting, sandeel, sprat, trisopterus sp., herring and sardine as potential preys. The shift of the abundance of porpoises form the northern parts of the North Sea to its southern parts was attributed to the sandeel abundance decline in the northern parts of the North Sea along with the re-invasion of the southern North Sea by the sardine species, probably in response to climate change. Finally, the value of a multi-approach dietary analysis was evaluated. Besides overcoming the limitations of each method, combining different techniques that integrate diet over days and weeks allowed gaining more complete understanding of harbour porpoise's diet.

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