A Taphonomic Comparison Between the Strait of Magellan and the Beagle Channel Andean Geology, Vol

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A Taphonomic Comparison Between the Strait of Magellan and the Beagle Channel Andean Geology, Vol Andean Geology ISSN: 0718-7092 [email protected] Servicio Nacional de Geología y Minería Chile Cárdenas, Javiera; Gordillo, Sandra Paleoenvironmental interpretation of late Quaternary molluscan assemblages from southern South América: A taphonomic comparison between the Strait of Magellan and the Beagle Channel Andean Geology, vol. 36, núm. 1, enero, 2009, pp. 81-93 Servicio Nacional de Geología y Minería Santiago, Chile Available in: http://www.redalyc.org/articulo.oa?id=173914379007 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Andean Geology 36 (1): 81-93. January, 2009 Andean Geology formerly Revista Geológica de Chile www.scielo.cl/rgch.htm Paleoenvironmental interpretation of late Quaternary molluscan assemblages from southern South America: A taphonomic comparison between the Strait of Magellan and the Beagle Channel Javiera Cárdenas1, 2, Sandra Gordillo3, 4 1 Fundación Centro de Estudios del Cuaternario (CEQUA), Av. Bulnes 01855, Punta Arenas, Chile. 2 Centro de Ciencias Ambientales EULA-Chile, Universidad de Concepción, Casilla 160-C, Barrio Universitario s/n, Concepción, Chile. [email protected] 3 Centro de Investigaciones en Ciencias de la Tierra, Consejo Nacional de Investigaciones Científicas y Técnicas (CICTERRA, CO- NICET), Av. Vélez Sársfield 1611, X5016GCA, 5000, Córdoba, Argentina. 4 Centro de Investigaciones Paleobiológicas (CIPAL), Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de Córdoba, Av. Vélez Sársfield 299, 5000, Córdoba, Argentina. [email protected] ABSTRACT. This study analyzes the Holocene molluscan assemblage in raised marine terraces along the coasts of the Strait of Magellan and the Beagle Channel. A total of 33 gastropods and 12 bivalves were identifi ed. They constitute the fi rst mollusk listing for deposits in the Strait of Magellan. Taphonomic analysis suggests a high energy environment with epifaunal elements in the Strait of Magellan and a low energy environment with the predominance of infaunal elements in the Beagle Channel. All the collected species are living taxa suggesting that postglacial climatic variations were not enough to alter the composition of the communities since at least 6,000 yr BP in the southern Chile-Argentina region. Keywords: Late Quaternary, Mollusks, Paleoecology, Taphonomy, Strait of Magellan, Beagle Channel, Chile, Argentina. RESUMEN. Interpretación paleoambiental de ensambles de moluscos del Cuaternario tardío del sur de América del Sur: una comparación tafonómica entre el Estrecho de Magallanes y el Canal Beagle. Este trabajo analiza los ensambles de moluscos del Holoceno de las terrazas marinas presentes a lo largo de las costas del Estrecho de Magallanes y del Canal Beagle. Un total de 33 especies de gastrópodos y 12 de bivalvos fueron identifi cados. Ellos constituyen un primer listado de moluscos para los depósitos del Estrecho de Magallanes. El análisis tafonómico sugiere un ambiente de alta energía con elementos epifaunales en el Estrecho de Magallanes y un ambiente de baja energía con el predominio de elementos infaunales para el Canal Beagle. Todas las especies colectadas son taxa vivientes, lo que sugiere que las variaciones climáticas postglaciales no fueron sufi cientes para alterar la composición de las comunidades desde al menos 6.000 años AP en el extremo austral de Chile-Argentina. Palabras claves: Cuaternario tardío, Moluscos, Paleoecología, Tafonomía, Estrecho de Magallanes, Canal Beagle, Chile, Argentina. 82 PALEOENVIRONMENTAL INTERPRETATION OF LATE QUATERNARY MOLLUSCAN ASSEMBLAGES FROM SOUTHERN SOUTH AMERICA... 1. Introduction occupied by outlet glaciers of an expanded southern Andean ice cap during successive Pleistocene gla- The southern tip of South America, Tierra ciations (Porter et al., 1992; Kilian et al., 2007). del Fuego, experienced the combined effects of Today, the strait is dominated by an indented rocky glaciations, changes in the sea level and inter- shoreline and characterized by semi-diurnal and rupted connectivity between the Atlantic and the heterogeneous tides with mean amplitudes ranging Pacifi c Ocean. Given that this area lies between both from 1.2 m on the west coast to 9 m in the Atlantic oceans, it is a critical region for the evaluation of inlet of the east coast (Andrade, 1991). paleoenvironmental changes and the interpretation Brambati et al. (1998) recognized four orders of faunal distributions in the Magellan Region (Gor- of marine terraces: I, II, III and IV order; with their dillo et al., 2008). Previous research in the Strait age estimations based on radiometric dating of fossil of Magellan and the Beagle Channel revealed that macrofauna. The selected localities for paleonto- marine events during the Pleistocene and Holocene logical samples correspond to fi ve sites previously are represented by marine terraces with altitudinal dated by Brambati et al. (1998): Bahía Porvenir differences resulting from glacio-isostatic effects (BP), Puerto del Hambre (PH), Punta Palo (PP), and the neotectonic uplift which occurred after the Punta Zeger (PZ) and Seno Otway (SO) (Table 1). Last Glacial Maximum (LGM) (Brambati et al., Beagle Channel . The Beagle Channel is located in 1998; Rabassa et al., 2000). the seismically active tectonic area of the Fuegian Quaternary marine deposits containing mainly Andes and was covered during the Last Glacial mollusks are extensively distributed along the Maximum. This channel is a glacial Andean valley, coasts of the Strait of Magellan and the Beagle occupied by the sea since 8,000 yr BP (Rabassa Channel (Rabassa et al., 1986; Gordillo et al., 1992; et al., 1986). It extends for 180 km long in a W-E Brambati et al., 1998). Previous studies along the trend linking the Atlantic and Pacifi c oceans along southern Tierra del Fuego coastline show that mol- the southern coast of Tierra del Fuego. The northern lusks are a key to reconstruct Holocene paleocom- Beagle Channel is characterized by a Holocene te- munities (Gordillo, 1999) and to evaluate changes rrace system with at least 3 orders of terraces at 10-8 in faunal composition after the LGM (Gordillo et m, 6-4 m and 3-1.5 m (Gordillo et al., 1992). Today, al., 2005). Interspecies variations existing in the the Beagle Channel, is dominated by an indented, fossil record are the result of a combination of rocky shoreline, with pocket gravel beaches. Tides life habits, intrinsic shell properties and habitat. are semi-diurnal with mean amplitudes of one me- In this way, taphonomic analyses may constitute a ter (e.g., 1.1 m at Ushuaia) (Gordillo et al., 1992). powerful tool for paleoenvironmental analyses of The selected study localities for paleontological Quaternary marine deposits (Brandt, 1989; Nielsen samples correspond to sites previously dated (Table and Funder, 2003). 1): Alakush (AK), Bahía Brown (BB, two levels), The objective of this study is to compare the Harberton (HA), Isla Gable (IG), Lago Roca (LR) Holocene molluscan assemblages located along and Ushuaia (US). the Strait of Magellan and the Beagle Channel coastlines by means of taxonomic, paleoecologic 2.2. Material studied and taphonomic analyses. 2.2.1. Taxa composition and paleoecology 2. Materials and Methods Fossil mollusks were collected from selected terraces in the Strait of Magellan and the Beagle 2.1. Study area Channel. Three samples of 10 dm3 bulk of sediment and biologic material were obtained from each terra- The coastal area examined in this study consists ce; samples were sieved in the fi eld using 1 mm and of 11 localities, with a total of 14 marine terraces 0.05 mm sieves to reduce volume. All specimens along the Strait of Magellan and the Beagle Channel were sorted, counted and identifi ed to the species le- (Fig. 1, Table 1). vel in the laboratory. Taxonomic and paleoecologic Strait of Magellan. The Strait of Magellan separates aspects of the mollusks were studied and examined. Patagonia from Tierra del Fuego. It was repeatedly The autoecological characterization of the fossil Cárdenas and Gordillo/ Andean Geology 36 (1): 81-93, 2009 83 Punta Zeger; PZ: Punta Palo; PP: Puerto del Hambre; PH: Ushuaia. Bahía Porvenir; US: BP: Lago Roca; LR: Isla Gable; IG: Harberton; HA: les from Strait of Magellan and Beagle Channel. fi Bahía Brown; BB: Alakush; AK: Seno Otway; SO: FIG. 1. Map of the localities sampled and stratigraphic pro 84 PALEOENVIRONMENTAL INTERPRETATION OF ATE UATERNARY MOLLUSCAN ASSEMBLAGES FROM SOUTHERN OUTH MERICA L Q S A ... (5) (4) (3) (1) (2) (3) (3) (6) cur- te cor- lled with fresh- fi 1986; (6) Gordillo, 1990. et al., Characteristics of the sampling sites References 1992; (4) Gordillo, 1991; (5) Rabassa et al., Ushuaia Peninsula. at present it is a freshwater lake disconnected from the open sea. nel into two branches forming its narrowest part. rent coast. It is constituted by a sandy substrate. land, constituted by southeast-trending bedrock ridges formed gravel. drumlin channel. responds to sand and gravel. are constituted mainly by gravel. order, Both deposits, III and IV gravelly and sandy deposits. that is also disconnected from the open sea at present. It is formed by a series of low, that is also disconnected from the open sea at present. It formed by a series of low, rounded bedrock hills, surrounded by interconnected depressions water. 8.0 This is a small embayment open to the east and protected from sea by 6.4 Although in the recent past this lake was part of a marine archipelago, 5.0 This 9 km long-island is located 70 east of Ushuaia and divides the Beagle Chan- 4.0 This bay is located about 50 km east of Ushuaia. 2.3 This deposit is located 9 km west of Estancia Harberton, lying on an ancient inter- 2.6 5.0Archipelago) This site is a raised beach located in an area (the so-called Cormoranes (m a.s.l.) Elevation AECV-876c AC-1060 AECV-648c 4,000-5,000 1.5The rocky coast of the main- Arenas.
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