Muricid boreholes in Pleistocene acorn barnacles from the Beagle Channel: trophic interactions during the Last Interglacial in southern South America

被引：8

作者：

Gordillo, Sandra ^{[1
,2
]}

机构：

[1] Consejo Nacl Invest Cient & Tecn, Ctr Invest Ciencias Tierra, CICTERRA, CONICET UNC, Cordoba, Argentina

[2] Univ Nacl Cordoba, Fac Ciencias Exactas Fis & Nat, Ctr Invest Paleobiol CIPAL, RA-5000 Cordoba, Argentina

来源：

ALCHERINGA | 2013年 / 37卷 / 04期

关键词：

Southern South America; Pleistocene; barnacles; muricid boreholes; predation; LEPSIELLA-VINOSA GASTROPODA; TIERRA-DEL-FUEGO; CIRRIPEDIA THORACICA; PREY SIZE; PREDATION; CHILE; EVOLUTION; GENUS; COMPETITION; QUATERNARY;

D O I：

10.1080/03115518.2013.792458

中图分类号：

Q91 [古生物学];

学科分类号：

0709 ; 070903 ;

摘要：

Acorn barnacles with boreholes were recovered from a Pleistocene marine deposit on Navarino Island, on the southern coast of the Beagle Channel. Balanomorph shells were identified as Balanus laevis (Bruguiere, 1789), and a few bear small round holes located generally on the middle or apical part of the parietal plates, thus suggesting that they represent the work of small muricid predators. If so, this study is the first record of drilling predation on fossil barnacles reported in southern South America.

引用

页码：479 / 486

页数：8

共 15 条

[1] Cannibalism in Holocene muricid snails in the Beagle Channel, at the extreme southern tip of South America: an opportunistic response?
Gordillo, Sandra
PALAEONTOLOGIA ELECTRONICA, 2013, 16 (01)
[2] Pleistocene marine calcareous macro-and-microfossils of Navarino Island (Chile) as environmental proxies during the last interglacial in southern South America
Gordillo, S.
Cusminsky, G.
Bernasconi, E.
Ponce, J. F.
Rabassa, J. O.
Pino, M.
QUATERNARY INTERNATIONAL, 2010, 221 (1-2) : 159 - 174
[3] The southernmost evidence for an interglacial transgression (Sangamon?) in South America. First record of upraised Pleistocene marine deposits in Isla Navarino (Beagle Channel, Southern Chile)
Rabassa, J.
Gordillo, S.
Ocampo, C.
Hurtado, P. Rivas
GEOLOGICA ACTA, 2008, 6 (03) : 251 - 258
[4] Vertebrate continental assemblage from the Last Interglacial in southern South America (Entre Rios, Argentina). Biostratigraphy and paleoenvironment
Soledad Ferrero, Brenda
Ignacio Noriega, Jorge
Brunetto, Ernesto
Nunez Otano, Noelia
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2017, 466 : 89 - 99
[5] Processing Activities and Differentiation of Bird Utilization During the Late Holocene in the Beagle Channel Region (Southern South America)
Tivoli, A. M.
INTERNATIONAL JOURNAL OF OSTEOARCHAEOLOGY, 2014, 24 (03) : 397 - 406
[6] Climatic and environmental changes during the middle to late Holocene in southern South America: A sclerochronological approach using the bivalve Retrotapes exalbidus (Dillwyn) from the Beagle Channel
Gordillo, Sandra
Brey, Thomas
Beyer, Kerstin
Lomovasky, Betina J.
QUATERNARY INTERNATIONAL, 2015, 377 : 83 - 90
[7] Morphological differences between 'subrugosa' and 'gregaria' morphs of adult Munida (Decapoda: Anomura: Galatheidae) from the Beagle Channel, southern South America
Tapella, Federico
Lovrich, Gustavo A.
JOURNAL OF THE MARINE BIOLOGICAL ASSOCIATION OF THE UNITED KINGDOM, 2006, 86 (05) : 1149 - 1155
[8] Paleoenvironmental interpretation of late Quaternary molluscan assemblages from southern South America: A taphonomic comparison between the Strait of Magellan and the Beagle Channel
Cardenas, Javiera
Gordillo, Sandra
ANDEAN GEOLOGY, 2009, 36 (01): : 81 - 93
[9] Chemical analyses of the earliest pigment residues from the uttermost part of the planet (Beagle Channel region, Tierra del Fuego, Southern South America)
Fiore, Danae
Maier, Marta
Parera, Sara D.
Orquera, Luis
Piana, Ernesto
JOURNAL OF ARCHAEOLOGICAL SCIENCE, 2008, 35 (12) : 3047 - 3056
[10] SEASONAL VARIATIONS IN SIZE, BIOMASS, AND ELEMENTAL COMPOSITION (CHN) OF HALICARCINUS PLANATUS (BRACHYURA: HYMENOSOMATIDAE) LARVAE FROM THE BEAGLE CHANNEL, SOUTHERN SOUTH AMERICA
Diez, Mariano J.
Spivak, Eduardo D.
Anger, Klaus
Lovrich, Gustavo A.
JOURNAL OF CRUSTACEAN BIOLOGY, 2012, 32 (04) : 575 - 581

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