Varios restos de aves marinas halladas en un nuevo yacimiento del Golfo de Bizkaia, situado en el estadio Atlántico, han proporcionado datos que ponen en evidencia el consumo humano de aves marinas y su influencia en su actual distribución geográfica

Antonio Sánchez Marco

Mikelo Elorza

Munibe Antropologia-Arkeologia

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MUNIBE (Antropologia-Arkeologia) Nº45 179-185 SAN SEBASTIAN 1993 ISSN 1132-2217 Aceptado: 1992-12-20 Postglacial fossil Great Auk and associated avian fauna from the Biscay Bay Fosil postglaciar de Alca Grande y avifauna asociada procedente del Golfo de Bizkaia KEY WORDS: Sea birds, Great auk, Palaeobiogeography, Palacoethnography, Holocene, Basque Country. PALABRAS CLAVE: Aves marinas, Alca grande, Paleobiogeografía, Paleoetnografía, Holoceno, País Vasco. Mikelo ELORZA * Antonio SANCHEZ MARCO** * Dpto. de Arqueología Prehistórica. Sociedad de Ciencias Aranzadi. 20003 Donostia. Spain. ** Museo Nacional de Ciencias Naturales. J. Gutiérrez Abascal, 2. 28006 Madrid. Spain. SUMMARY Sea bird remains found in a new Atlantic stage settlement located in the Basque coast have yielded conclusive data concerning the human comsuption on these birds, and the anthropic influence on their present geographical distribution. RESUMEN Varios restos de aves marinas halladas en un nuevo yacimiento del Golfo de Bizkaia. situado en el estadio Atlántico, han proporciona- do datos que ponen en evidencia el consumo humano de aves marinas y su influencia en su actual distribución geográfica. LABURPENA Bizkaiko golkoko aztarnategi berri batean aurkitutako itsas-hegaztien aztarnak. Atlantiar garaian koka daitezkeenak. gizonaren elikadura- rako erabiliak izan zirela ziurtatu dute. eta kontsumorako erabilpen honek, hegazti hauen gaurko zabalkunde geografikoan eduki duen eragi- na adierazi dute. INTRODUCTION As a consequence of a rescue excavation under- taken in a layer —threatened with imminent destruc- tion by building works— containing remains of human occupation, a relevant collection of bird fossil bones was exhumed. Radiometric analysis and lithic arti- facts studies conclude that the settlement is to be attributable to the early Neolithic. Special importance of this locality lies in the set of seabirds species present. Particularly remarkable is the occurrence of the great auk —Pinguinus impen- nis (L., 1758)—. Together with the fossil remains, mammal ones as well as pollen, foraminifera and lithic tools have been found at Herriko Barra, which yield a compre- hensive scene of the local environment conditions and the corresponding human behaviour. SITE DESCRIPTION AND STRATIGRAPHY The site, known as Herriko Barra, is located on the Bay of Biscay, in the town of Zarautz, Basque Country coast (Fig. 1), lat. 43.17 N, long. 2.10 E. The local holocene sediments extend on an area of ca. 2 km2 opened to the Cantabrian sea and fairly delimi- ted by a series of three minor hills. An unique fertile layer appears included in a stra- tigraphic profile where ALTUNA et alii (in press) distin- guished six sedimentary beds (Fig. 2): from A, on the base, to F, on the top. Inquiries into the depositional processes of the sediments have revealed signs of two marine transgressions in under and overlaying beds A and E, which have been respectively identi- fied with the transgressive episodes Flandrian and Dunkerkian. The remains, the subjet of this work, were exhumed from the stratum labeled C, which shows a regular thickness of ca. 40 cm. Sediments of this stratum show a blackish color owing to their richness of organic materials. Traces of edaphic pro- cesses can be also observed here (ALTUNA et alii, in press). 180 M. ELORZA &A. SANCHEZ MARCO Figure 1. Geographical location of the deposit of Herriko Barra. Figure 2. Section-diagram of the deposit of Herriko Barra showing the stratigraphic sequence analysed and the radiocarbon dating carried out. POSTGLACIAL FOSSIL GREAT AUK AND ASSOCIATED AVIAN FAUNA FROM THE BISCAY BAY 181 Absolute datations have been calculated by the laboratory Teledyne Isotopes (New Jersey, USA) on the proportions of 14C in vegetal material carried out from the underlaying bed B, just from a point very close to the layer C. The results offer a chronology of 5.810 ± 170 BP. Some characters of the unit C, e.g. the abundan- ce of plant fragments as well as traces of bioturba- tion, might be interpreted as evidence of holocene pedogenetic processes. These sediments have revea- led themselves as a very good conservative medium for grains of pollen. Among the trees, which always maintain a proportion of not less than 50% non-arbo- reous plants, the dominant species are Alnus, Corylus, Pinus and secondarily Quercus. Study of the pollen points to the Atlantic stage (ALTUNA et alii, in press). The mammal fauna remains consist predomi- nantly of Cervus elaphus, with occurrence of other ungulates as the roe deer, wild boar and aurochs as well as carnivores and insectivores: bear, wolf, bad- ger and hedgehog. The occurrence of a fawn aged one month should indicate that the site was occu- pied at least at the end of the spring and the begin- ning of the summer (ALTUNA et alii, in press). AVIAN SURVEY The layer C of Herriko Barra has recorded a taxo- nomically and biotypically homogeneous portion of the contemporaneous ornithofauna. The fossil mate- rial is displayed in table 1, where following abbrevia- tions are used: hum - humerus uln -ulna rad -radius cmc - carpometacarpus cor - coracoid str -sternum fur -furcula tbt - tibiotarsus pha -phalange sin -left dex - right dia - diaphisis pro - proximal dis - distal cra -cranial cau -caudal juv -juvenile A complete carpometacarpus of Fulmarus glacia- lis has been recorded (measurements in Table 2), which shows a distinctive feature respecting Puffinus, Pterodroma and Laridae, having the facets for digits II and III at the same level. Likewise, the in- ner edge of the carpal trochlea has a peculiar sinuo- sity. Table 1. List of species and remains found at Herriko Barra Fulmarus glacialis: cmc dex (burnt?) Puffinus puffinus: cmc sin dis Grus grus: tbt sin dis juv Rissa tridactyla: cor sin Pinguinus impennis: hum sin pro hum sin dis hum dex juv uln dex dis cmc sin Alca torda: hum sin dis uln sin pro cor sin cau cor dex cau (burnt) 3 str cra Uria aalge: 4 hum dex pro 3 hum dex dia hum sin pro 5 hum dex dis 3 hum sin dis 5 hum sin dia 2 hum sin pro 2 uln dex pro uln sin pro uln dex dis fur cor sin cra 3 cor dex cra (2 burnt) 2 cor dex cau cor sin cau tbt sin pro tbt sin dis tbt dex dis pha 1 (a) digit major dex Fratercula arctica: 2 hum dex pro hum dex dia (burnt) uln sin pro rad sin pro cmc dex pro cor sin Table 2. Measurements of F. glacialis (taken after MOURER- CHAUVIRÉ, 1975). 1 3 4 5 6 60.0 4.3 7.2 4.6 3.6 182 M. ELORZA & A. SANCHEZ MARCO The bones of F. glacialis and Rissa tridactyla (mea- surements in Table 3) from Herriko Barra constitute the earlier finds of these species from the Iberian Peninsula. Table 3. Measurements of R. tridactyla (taken after MOURER- CHAUVIRÉ, 1975). 1 3 6 33.4 8.3 4.4 The occurrence of the extinct great auk (Pingui- nus impennis (L., 1758)) in any outcrop is of major importance. Five fragments of fossilized bones have been recovered from the settlement of Herriko Barra (Tabs. 1, 4 and Fig. 3). Table 4. Measurement in mm of P. impennis (taken after MOURER- CHAUVIRÉ, 1975). excepting 2b: from the ventral tubercle to the pectoralis impression, and 6b: depth (orthogonal to 6). BMNH are specimens of the British Museum (Nat. Hist.), D.T. corresponds to the Devil's Tower's specimen. PALAEOETHNOGRAPHIC INTEREST Variuos facts support the thesis that birds were incorporated into the diet of the human group that frequented the Herriko Barra site: (1) It is difficult to explain the observed avian taphocaenoses in an open air settlement otherwise than by accepting hu- man interference. (2) The major representation of skeletal elements lies on those limb bones bearing the most voluminous muscles, with the highest nu- tritional value. This kind of representation characteri- zes the remains of animals used as food in human settlements (cf. MOURER-CHAUVIRÉ, 1983). (3) Two cut-marks can be observed on the humerus of the ju- venile great auk, (Fig. 4) situated between the fora- men nutritium and the inner crest, probably made with a sharped tool in flint. (4) It is also to be noticed the existence of evidence of burning on four bones, maybe on five (see Tab. 1). It is historically and archaeologically well docu- mented that until modern times seabirds —including the great auk until its definitive extinction— have been used as food (e.g. GREENWAY, 1967 and SERJEANTSON, 1988). At the mesolithic site of Téviec (PÉQUART et alii, 1937), among the kitchen scraps —molluscs and crustaceans mostly— abandoned the- re, a noteworthy number correspond to seabirds, which seem to have been exploited as food resour- ces. The capture of great auks is likewise the inter- pretation suggested in the study of Figueira Brava (cf. MOURER-CHAUVIRÉ & ANTUNES, 1991). The inhabitants of Herriko Barra consumed these birds as a complement of mammals. There is no evi- dence that man's avian preys included other than sea- birds, indubitably present in the surroundings. This offers an interesting specialization in this area of South Europe. PALAEOBIOGEOGRAPHY The seabirds found in Herriko Barra are current wintering and birds of passage in the Cantabric coast. Solely Rissa tridactyla breeds, Uria aalge persevere in a recessive breeding, and breeding of Fulmarus glacialis has still to be confirmed (BARCENA, TEIXEIRA & BERMEJO, 1984). In the Bay of Biscay some of them (RIOFRIO, 1988) can be observed during migration and western storms, but they do not breed in the Basque Country. The settlement was frequented at least at the end of spring and the beginning of summer (ALTUNA et alii, in press). Some of these species, concretely Ful-marus glacialis, Uria aalge; Alca torda and Rissa tridactyla, often breed jointly (VOOUS, 1960). This fact opens the possibility that these species held bree- ding status at the time of human's settlement. As said, absolute datations and palinological evi- dences (ALTUNA et alii, in press) place the settlement in the Atlantic stage, so we can reject the possibility of a colder climatic situation that pushed these birds to breed more southerly than their current breeding places in Europe, which are north to 45º N. The ex- planation of their presence in Herriko Barra is given by the literature generated by Pinguinus impennis's findings. POSTGLACIAL FOSSIL GREAT AUK AND ASSOCIATED AVIAN FAUNA FROM THE BISCAY BAY 183 Figure 3. Remains of Pin- guinus impennis from Herriko Barra. Figure 4. Cut-marks on the humerus of a juvenile Pinguinus impen- nis from Herriko Barra. Direct vestiges of these extint bird have been lo- cated at some sites of the southern part of the Iberian Peninsula. Thus, mousterian sediments of Devil's Tower yielded two fragments of humeri (BATE, 1928). Likewise, very close to this site, two specimens belonging to the great auk were recove- red from a mousterian layer at Gorham's Cave (EASTHAM, 1968), as well as five fossil bones from the Epipaleolithic of Cueva de Nerja (BOESSNECK & DRIESCH, 1980) and one sternum from a magdalenian bed of this same local stratigraphy (EASTHAM, 1986). Iterative attention has been given to a drawing in the cave of El Pendo, province of Santander, considered as an earlier representation of the great auk (BREUIL, ALCALDE DEL RIO and SIERRA, 191 2, GONZALEZ MORALES, 1980). Most recently, MOURER-CHAUVIRÉ and ANTUNES (1991) have published the finding of new remains —two fragments of two humeri— at Gruta da Figueira Brava (Serra da Arrábida, Portugal), in a sandy bed dated by 14C to 30,930 ± 700 BP (ICEN-387) (fide ANTUNES et alii, 1989), which overlies marine layers ascribed to the Thyrrenian III. At the time when the sediments of Devil's Tower were depositing, the great auk enlarged its geographical distribution eastwards and reached the region of Calabria (Southern Italy): a fragment of ti- biotarsus was recorded at Archi (ASCENZI & SEGRE, 1971). Not far from there, in Grotta Romanelli (region of Puglia), BLANC (1927) reports this species —one hu- merus and one femur (LACORTE, 1990)— in levels da- 184 M. ELORZA & A. SANCHEZ MARCO ted by 14C between 11,600 and 9,800 BP (fide CASSOLI, SEGRE & SEGRE, 1977). More recent —from a mesolithic, or possibly paleolithic, layer— is the radius identified at Arene Candide (region of Liguria) (CASSOLI, 1980). The most southerly point in the Palaearctic region is given by the occurrence of an sternum in Porto Santo (archipelago of Madeira) (PIEPER, 1985). Pinguinus impennis has been considered an in- habitant of Holarctic northern seas. That is certain for the last centuries of its existence, but Figure 5 shows that this bird had a much more moderate cli- matic distribution. There are findings from the Holocene in Herriko Barra, Arene Candide and Nerja, places where a bird considered strictly arctic would not easily live. This thesis about great auk's sou- therly distribution was proposed by D.M.A. BATE (1928) in her comments on the Devil's Tower avifau- na. Human predation on this flightless species pro- bably caused its recession during the Holocene, until its extinction in Iceland. The influence of man upon seabirds and their eggs has caused throughout his- tory a severe reduction of many bird populations: If we applied this fact, the avifauna found at Herriko Barra could therefore be considered as an indicator of a biogeographic past disturbed by human action. BIBLIOGRAPHY ANDREWS, C.W. 1920 Remains of the Great Auk and Ptarmigan in the Channel Islands. Ann. Mag. Natur. Hist. 9 s., 6 (2): 166. ALTUNA, J.; CEARRETA, A.; EDESO, J.M.; ELORZA, M.; ISTU- RITZ, M.J.; MARIEZKURRENA, K.; MUJIKA, J.A. & UGARTE, F. (in press) El yacimiento de Herriko-Barra (Zarautz, País Vasco) y su relación con las transgresiones marinas holocenas. Cuaternario y Geomorfología. Madrid. Figure 5. Sightings and remains of Pinguinus impennis. (See bibliography). POSTGLACIAL FOSSIL GREAT AUK AND ASSOCIATED AVIAN FAUNA FROM THE BISCAY BAY 185 ANTUNES, M.T.; CABRAL, J.P.M.; CARDOSO, J.L.; PAIS, J. &SO- ARES, A.M. 1989 Paleolítico médio e superior em Portugal: datas 14C, esta- do actual des conhecimentos, síntese e discussao. Ciências da Terra 10, 127-138. ASCENDI, A. & SEGRE, A. 1971 Il giacimento con mandibola neandertaliana di Archi (Reggio Calabria). Rendiconti Clase Sc.fis.mat.nat. ser. 8, 50 (6), 763-771. BARCENA, F.; TEIXEIRA, A.M. & BERMEJO, A. 1984 Breeding Seabird Populations in the Atlantic Sector of the Iberian Peninsula. ICBP Technical Publication 2, 335-345. BATE, D.M.A. 1928 The animal remains. In.: L.H.D. BUXTON, G.E. SMITH & D.M.A. BATE: «Excavations of a Mousterian rock-shelter at Devil's Tower, Gibraltar». Journal of the Royal Anthropology Institute 58, 92-111. BLANC, G.A. 1927 Sula presenza di Alca impennis Linn. nella formazione pleistocenica superiore di Grotta Romanelli in Terra d'Otrante. Archivo per l'Antropologia e Etnologia 58 (1-4), 34 PP. B0ESSNECK, J. &VON DEN DRIESCH, A. 1980 Tierknochenfunde aus vier südspanischen Höhlen. Studien über frühe Tierknochenfunde von der Iberischen Halbinsel 7, 1-83. München. BREUIL, H.; ALCALDE DEL RIO, H. &SIERRA, L. 1912 Les cavernes de la Région Cantabrique (Espagne). A. Chêne Ed. 265 pp. Monaco. CASSOLI, P.F. 1980 L'avifauna del pleistocene superiore delle Arene Candide (Liguria). Memoria del'Istituto Italiano di Paleontologia Umana 3, 155-234. CASSOLI, P.F. & SEGRE, A.G. 1989 L'Alca impenne Alca impennis del Pleistocene d'Italia. Atti III Conv. Ital. Orn., 251-254. CASSOLI, P.F.; SEGRE, A.G. & SEGRE, E. 1977 Evolution morphologique et écologique de la côte de Castro (Pouilles) dans le Pléistocène final. In.: D. SONNEVI- LLE-BORDES: «La fin des temps glaciaires en Europe, 32. Colloques Internationaux C. N.R.S. 271. EASTHAM, A. 1968 The avifauna of Gorham's Cave, Gibraltar. Bulletin of the London Institute of Archeology 7, 37-42. 1986 The birds of the Cueva de Nerja. In.: J.F. JORDA (ed.): «La prehistoria de la Cueva de Nerja (Málaga)». Patronato de la Cueva de Nerja: 109-131. GONZALEZ MORALES, J.A. 1980 Interpretación ornitológica de los grabados. In.: J. GONZALEZ ECHEGARAY: El yacimiento de la cueva de "El Pendo" (Excavaciones 1953-57). Bibliotheca Praehistorica Hispana XVII, 257-261. GREENWAY, J.C. 1967 Extinct and Vanishing Birds of the World. Dover Publ., 520 pp. New York. LACORTE, E. 1990 Studio del paleoambiente del Salento attraverso i materiali fossili conservati nel Museo di Paleontologia di Maglie. Edizione Scientifique Museo Comunale Paleontologia Maglie 4, 109 pp. MELDGAARD, M. 1988 The Great Auk, Pinguinus impennis (L.) in Greenland. Historical Biology 1, 145-178. MOURER-CHAUVIRÉ, C. 1975 Les oiseaux du Pléistocène moyen et supérieur de France. Documents du Laboratoire de la Faculté de Sciences de Lyon 64 (2 fasc.), 624 pp. 1983 Les oiseaux dans les habitats paléolithiques: gibier des hommes ou proies des rapaces? Animal and Archaeology 2, 111-124. MOURER-CHAUVIRÉ, C. & ANTUNES, M.T. 1991 Présence du grand pingouin, Pinguinus impennis (Aves, Charadriiformes) dans le Pléistocène du Portugal. Geobios 24 (2). 201-205. PÉQUART, M.; PÉQUART, S.J.; BOULE, M. & VALLOIS, H. 1937 Téviec, station-nécropole mésolithique du Morbihan. Archives de l'Institut de Paléontologie Humaine 18, 227 PP. PIEPER, H. 1985 The fossil land birds of Madeira and Porto Santo. Bocagiana 88, 1-6. RIOFRIO, J. 1988 Migración de las aves marinas por el Cabo de Higer. Otoño 1984. Munibe (Ciencias Naturales -Natur Zientziak) 40, 55-72. SERJEANTSON, D. 1988 Archaeological and ethnographic evidence for seabird ex- ploitation in Scotland. Archaeozoologia II (2). 209-224. VOOUS, K.H. 1960 Atlas of European Birds. Nelson ed. 248 pp. 

Postglacial fossil Great Auk and associated avian fauna from the Biscay Bay.

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Postglacial fossil Great Auk and associated avian fauna from the Biscay Bay.

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