Powiadomienia systemowe
- Sesja wygasła!
- Sesja wygasła!
- Sesja wygasła!
Tytuł artykułu
Treść / Zawartość
Pełne teksty:
Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
La Meseta Formation is made up of estuarine and shallow marine, fossiliferous clastic deposits 720 m thick that provides a unique record of marine and terrestrial biota of Antarctic ecosystems preceding continental glaciation in the Oligocene. The lower limit of this formation has been poorly known, and therefore it has been carefully investigated. The lowest part of the La Meseta Formation, at the southern bank of a palaeodelta, is represented by relics of a prograding sequence of sediments deposited in the wave-dominated part of a deltaic system in the offshore and lower and upper shoreface environments. The sequence is completed landwards by younger tidal plain sediments deposited at 40 m lower altitude in a relatively protected, central estuarine basin, which was dominated by tidal activity and influenced by periodic fluvial inflow. These strata were deposited during a late Paleocene or Ypresian/Lutetian lowstand of sea level, which might reflect a glaciation event or glacioisostatic rebound of land following deglaciation of hypothetic Antarctic inland glaciers. Forced regression of sea level and seaward expansion of a deltaic freshwater environment, led to local extinction of a unique assemblage of marine echinoderms, bryozoans, corals and brachiopods. These marine fossils, representing a thanatocoenosis, are perfectly preserved due to syngenetic goethite permineralisation. This process owed its origin to excess reactive iron coming from sulphide-rich bedrock through weathering processes and acid sulphate drainage of the neighbouring land area.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
345--360
Opis fizyczny
Bibliogr. 77 poz.,
Twórcy
autor
autor
autor
- Department of Antarctic Biology, Polish Academy of Sciences, Ustrzycka 10/12, PL-02-141 Warszawa, Poland, ta tura@interia.pl
Bibliografia
- 1.AMINI Z. Z., ADABI M. H., BURNETT C. F. and QUILTY P. G. (2004) - Bryozoan distribution and growth form associations as a toolin environ mental interpretation, Tasmania, Australia. Sediment. Geol., 167: 1-15.
- 2.ASKIN R. A. (1988) - Campanian to Paleocene palynological succession of Sey mour Island and adjacent islands, north eastern Antarctic Peninsula. Geol. Soc. Am. Mem., 169: 131-153.
- 3.ASKIN R. A. (1993) - Palynology of an olistrostrome at Cape Wiman, Seymour Island. Antarctic J. United States, Rev., 28 (5): 49-50.
- 4.BAUMILLER T. K. and GAZDZICKI A. (1996) - New crinoids from the Eocene La Meseta Formation of Sey mour Island, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic Expeditions (ed. A. Gaüdzicki). Part II. Palaeont. Pol., 55: 101-116.
- 5.BEU A. G. (2009) - Before the ice: biogeography of Antarctic Paleogene molluscan faunas. Palaeogeogr. Palaeoclimat. Palaeoecol., 284: 191-226.
- 6.BIJL P. K., SCHOUTEN S., SLUIJS A., REICHART G. J., ZACHOS J. C. and BRINKHUIS H. (2009) -Early Palaeogene temperature evolution of the south west Pacific Ocean. Nature, 461 (7265): 776-779.
- 7.BITNER M. A. (1996) - Brachiopods from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic Expeditions (ed. A. Gazdzicki). Part II. Palaeont. Pol., 55: 65-100.
- 8.BIRKENMAJER K., GAZDZICKI A., KRAJEWSKI A., PRZYBYCIN A., SOLECKI A. and TATUR A. (2005) - First Cenozoic glaciers in West Antarctica. Pol. Polar Res., 26 (1): 3-12.
- 9.BOIKO N. I. (2001) - Lithofacies features and formation conditions of rocks in the Azov-Kuban Region. Lithol. Miner. Res., 36 (2): 156-159.
- 10.CAMERON B. (1967) - Fossilization of an ancient (Devonian) soft-bodied worm. Science, 155 (3767): 1246-1248.
- 11.CASE J. A. (2006) - The late Mid dle Eocene terres trial vertebrate fauna from Seymour Island: the tails of the Eocene Patagonian size distribution. Geol. Soc. London, Spec. Publ., 258: 177-186.
- 12.COCOZZAC D. and CLARKEC M. (1992) - Eocene microplankton from La Meseta Formation, north ern Seymour Island. Antarctic Sc., 4: 355-362.
- 13.DOKTOR M., GAZDZICKI A., JERZMANSKA A., POREBSKI S. J. and ZASTAWNIAK E. (1996) - A plant-and-fish assemblage from the Eocene La Meseta Formation of Seymour Island (Antarctic Peninsula) and its environmental implications. Palaeont. Pol., 55: 127-146.
- 14.DOKTOR M., GAZDZICKI A., MARENSSI S. A., POREBSKI S. J., SANTILLANA S. N. and VRBA A. V. (1988) - Argentine-Polish geological investigation on Seymour (Marambio) Island, Antarctica, 1988. Pol. Polar Res., 9 (4): 521-541.
- 15.ELLIOT D. H. (1988) - Tectonic setting and evolution of the James Ross Basin, northern Antarctic Peninsula. Geol. Soc. Am. Mem., 169: 543-555.
- 16.ELLIOT D. H. (1993) - Geological studies at Cape Wiman, Seymour Island. Antarctic J. Rev.: 48-49.
- 17.ELLIOT D. H., RINALDI C., ZINSMEISTER W. J., TRAUTMAN T. A., BRYANT W. A. and del VALLE R. (1975) - Geological in vestigations on Seymour Island, Antarctic Peninsula. Antarctic J. United States, 10 (4): 182-186.
- 18.ELLIOT D. H. and TRAUTMAN T. A. (1982) - Lower Tertiary strata on Seymour Island, Antarctic Peninsula. In: Antarctic Geoscience (eds. C. Craddock and I. B. Camp bell): 297-297. The University of Wisconsin Press, Madison.
- 19.FERNÁNDEZ-REMOLAR D. C. and KNOLL A. H. (2008) - Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: Implications for Mars exploration. Icarus, 194 (1): 72-85.
- 20.GANDOLFO M. A., MARENSSI S. A. and SANTILLANA S. N. (1998) - Floray paleoclima de la formation La Meseta (Eoceno Medio), Isla Marambio (Seymour), Antartida. Ass. Paleont. Argentina, Publ. Especial, 5: 155-162.
- 21.GAZDZICKI A. and HARA U. (1994) - Multilamellar Bryozoan colonies from the Eocene La Meseta Formation of Seymour Island, Antarctica: a preliminary account. Stud. Geol. Pol., 104: 105-116.
- 22.GAZDZICKI A., HARA U. and TATUR A. (2004) - The Weddell Sea Formation. Pol. Polar Res., 25: 189-204.
- 23.GAZDZICKI A. and TATUR A. (1994) - New place names for Seymour Island (Antarctic Peninsula) introduced in 1994. Pol. Polar Res., 15 (1-2): 82-85.
- 24.HALLAM A. and WIGNALL P. B. (1999) - Mass extinctions and sea-level changes. Earth Sc. Rev., 48 (4): 217-250.
- 25.HARA U. (1997a) - Bryozoan assemblages from the La Meseta Formation (Eocene) of Seymour Island Antarctic Peninsula. In: The Antarctic Region: Geological Evolution and Processes (ed. C. A. Ricci): 1001-1006. Terra Antarctica Publ., Sienna.
- 26.HARA U. (1997b) - Tertiary bryozoans of West Antarctica and their ecological and biogeographical implications. In: Polish Polar Studies. 24th Po lar Symposium, Warszawa, 1997 (ed. P. Głowacki): 115-140. Inst. Geoph. Pol. Acad. Sc., Warszawa.
- 27.HARA U. (2001) - Bryozoans from the Eocene of Seymour Island, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic Expeditions (ed. A. Gaździcki). Part III. Palaeont. Pol., 60: 33-156.
- 28.HAQ B. U., HARDENBOL J. and VAIL P. R. (1987) - Chronology of fluctuating sea level since the Triassic. Sci ence, 235: 1156-1167.
- 29.HAQ B. U., HANDERBOL J. and VAIL P. R. (1988) - Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level changes. In: Sea-level Changes: an Integrated Approach (ed. K. W. Wilgus et al.). SEPM Spec. Publ., 42: 71-108.
- 30.HAUGH B. H. and BELL B. M. (1980) - Fos sil ized Vis cera in Primitive Echinoderms. Science, 209 (4457): 653-657.
- 31.HUTCHNINIGS P., AHYONG S., BYRE M., PRZESLAWSKI R. And WORHEIDE G. (2009) - Part II Species and species groups. Chapter 11. Vulnerability of benthic in vertebrates of the Great Barrier Reef to climate change: 310-356
- 32.IVANY L . C., LOHMANN K. C., HASIUK F., BLAKE D. B., GLASS A., ARONSON R. B. and MOODY R. (2008) - Eocene climate record of a high southern latitude continental shelf: Seymour Is land, Antarctica. Geol. Soc. Am. Bull., 120: 659-678.
- 33.LONG D. J. (1992) - Paleoecology of Eocene Antarctic sharks. In: The Antarctic Paleoenvironment: a Perspective on Global Change (eds. J. P. Ken nett and D. A. Warnke). Part I. Antarctic Res. Ser., 56: 131-139.
- 34.MACELLARI C. E. (1988) - Stratigraphy, sedimentology and paleoecology of Upper Cretaceous/Paleocene shelf sediments of Seymour Island. Geol. Soc. Am. Mem., 169: 25-53.
- 35.Mac GINITLE (1939) - Some effects of fresh water on the fauna of marine harbor. Am. Midland Natur., 21 (3): 681-689.
- 36.MANI K. (1996) - Permineralization Re trieved March 29, 2009, from Fossils: a window to the past. Website: http://www.ucmp.berke - ley.edu/paleo/fos sils/permin.html
- 37.MARENSSI S. A. (2006) - Eustatically con trolled sedimentation recorded by Eocene strata of the James Ross Basin. Antarctica Geol. Soc., London, Spec. Publ., 258: 125-133.
- 38.MARENSSI S. A., NET L. I. and SANTILLANA S. N. (2002) - Provenance, environmental and paleogeographic controls on sandstone composition in an incised-valley system: the Eocene La Meseta Formation, Seymour Island, Antarctica. Sediment. Geol., 150: 301-321.
- 39.MARENSSI S. A., REGUERO M. A., SANTILLANA S. N. And VIZCAINO S. F. (1994) - Review. Eocene mammals from Seymour Island, Antarctica: palaeobiogeographical implications. Antarctic Sc., 6 (1): 3-15.
- 40.MARENSSI S. A., SANTILLANA S. N. and RINALDI C. A. (1998a) - Paleoambientas sedimentarios de La Aloformation La Meseta (Eoceno), Isla Marambio (Sey mour). Contribucion Cientifica del Instituto Antartico Argentino, 464: 1-51.
- 41.MARENSSI S. A., SANTILLIANA S. N. and RINALDI C. A. (1998b) - Stratigraphy of the La Meseta Formation (Eocene) Marambio (Seymour) Island, Antarctica. Ass. Paleont. Argen tina, Publ. Especial, 5: 137-146.
- 42.NAWROCKI J., PANCZYK M. and WILLIAMS J. S. (2010) - Isotopic ages and palaeomagnetism of selected magmatic rocks from King George Island (Antarctic Peninsula). J. Geol. Soc., London, 167: 1063-1079.
- 43.PAINE M. (2005) - Sedimentology of the Bondi Main heavy mineral beach placer deposit, Murray Basin, south eastern Australia. Sediment. Geol., 174 (3-4): 177-195.
- 44.PAYROS A., TOSQUELLA J., BERNAOLA G., DINAROS-TURELL J., ORUE-ETXEBARRIA X. and PUJALTE V. (2009) - Filling the North European Early/Mid dle Eocene (Ypresian/Lutetian) boundary gap: insights from the Pyreneancontnental to deep-ma rine record. Palaeogeogr. Palaeoclimat. Palaeoecol., 280 (3-4): 313-332.
- 45.PIRRIE D., DITHFIELD P. W. and MARSHALL J. D. (1994) - Burial diagenesis and pore-fluid evo lution in a Mesozoic backarc ba sin: the Marambio Group, Vega Island, Antarctica. J. Sediment. Res. A, 64: 541-552.
- 46.PFRETZSCHNER H. U. (2001) - Iron oxides in fossilbone. Neues Jahrb. Geol. Paläont., Abh., 220: 417-429.
- 47.POREBSKI S. J. (1995) - Facies architecture in a tectonically-controlled in cisedval ley es tu ary: La Meseta For ma tion (Eocene) of Sey mour Island, Ant arc tic Pen in sula. Stud. Geol. Pol., 107: 7-97.
- 48.POREBSKI S. J. (2000) - Shelf-val ley com pound fill pro duced by fault subsidence and eustatic sea-level changes, Eocene La Meseta Formation, Seymour Island, Antarctica. Geology, 28: 147-150.
- 49.PROTHERO D. R. and BERGGREN W. A. (1992) - Eocene-Oligocene climatic and biotic evolution. Prince ton University Press.
- 50.RADWANSKA U. (1996) - A new chinoid from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic expeditions. Part II. (ed. A. Gaüdzicki). Palaeont. Pol., 55: 117-125.
- 51.REGUERO M. A., VIZCAINO S. F., GOIN F. J., MARENSSI S. A. And SANTILLANA S. N. (1998) - Eocene highlattude terres trial vertebrates from Antarctica as biogeographic evidence. Asoc. Paleont. Argentina. Publ. Especial, 5: 185-198.
- 52.RINALDI C. A., MASSABIE A., MOERLLI J., ROSENMANN L. H. And del VALLE R. A. (1978) - Geologia de la isla Vicecomodoro Marambio, Anartida. Contribucion Cientifica del Instituto Antartico Argentino, 217: 1-37.
- 53.SADLER P. M. (1988) - Geometry and stratification of upper most Cretaceous and Paleogene units on Seymour Island, northern Antarctic Peninsula. Geol. Soc. Am. Mem., 169: 303-320.
- 54.SCHOPF J. M. (1975) - Modes of Fossil Preservation. Rev. Palaeobot. Palynol., 20: 27-53.
- 55.SCHWEITZER C. E., FELDMANN R. M., MARENSSI S. and WAUGHD. A. (2005) - Remark ably preserved annelid worms from the La Meseta Formation (Eocene), Seymour Island, Antarctica. Palaeontology, 48: 1-13.
- 56.SNEDDEN J. W. and LIU C. (2010) - A Compilation of Phanerozoic Sea-Level Change, Coastal Onlaps and Recommended Sequence Designations. Search and Discovery Article 40594.
- 57.STILWELL J. D. and ZINSMEISTER W. J. (1992) - Mollus can systematics and Biostratigraphy: Lower Tertiary La Meseta Formation, Seymour Island, Antarctic Peninsula. Antarctic Res. Ser., 55: 1-192
- 58.STOLARSKI J. (1996) - Paleogene corals from Seymour Island, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic Expeditions. Part I1 (ed. A. Gaździcki). Palaeont. Pol., 55: 501-506.
- 59.STOLARSKI J. (1998) - Conopora (Stylasteridae, Hydrozoa) from the Eocene of Sey mour Island. Ant arc tic Sc., 10 (4): 487-492.
- 60.SZCZECHURA J. (2001) - Ostracods from the Eocene of Seymour Is land, Antarctic Peninsula. In: Palaeontological Results of the Polish Antarctic Ex pedition. Part III. (ed. A. Gazdzicki). Palaeont. Pol., 60: 157-181.
- 61.TATUR A., BARCZUK A., del VALLE R., SLETTEN R. and KICINSKA E. (1993) - Surface mineralization on Seymour Island, Antarctica. Pol. Polar Res., 14 (2): 153-168.
- 62.THORN V. C. and DECONTO R. (2006) - Ant arctic climate at the Eocene/Oligocene bound aryclimate model sensitivity to highlatitude vegetation type and comparisons with paleobotanical record. Palaeogeogr. Palaeoclimat. Palaeoecol., 231: 134-157.
- 63.UHL D. and MONTENARI M. (2011) - Charcoal as evidence of palaeowildfires in the Late Triassic of SW Ger many. Geol. J., 46: 34-41.
- 64.VANHOVE D., STASSEN P., SPEIJER R. P. and STEURBAUT E. (2011) - Assessing paleotemperature and sea sonality during the early Eocene The facies and biota of the oldestexposed strata of the Eocene La Meseta Formation (Seymour Island, Antarctica) 359 climatic opti mum (EECO) in the Belgian basin by means of fish otolithstable O and Cisotopes. Geol. Belgica, 14 (3-4): 143-158.
- 65.Van WOESIK R., de VANTIER L. and GLAZEBROOK J. (1995) - Effects of Cyclone "Joy" on nearshore coral communities of the Great Barrier Reef. Mar. Ecol. Progress Ser., 128: 261-270.
- 66.VISCAINO S. F., REGUERO M. A., GOIN F. J., TAMBUSSI C. P. and NORIEGA J. I. (1998) - Community structure of Eocene terres trial vertebrates from Antarctic Peninsula. Asoc. Paleontol. Argentina. Publ. Especial, 5: 177-183.
- 67.WEIDLER P. G., SCHWINN T. and GAUB H. E. (1996) - Vicinal faces on synthetic goethite ob served by atomic force microscopy. Clay and clay Miner., 44 (4): 437-442.
- 68.WISE B. R. (1980) - Wave-dominated delta systems of the Upper Cretaceous San Miguel Formation, Maverick Basin, South Texas. Bureau of Economic Geology, Rep. Investigat., 107. Austin, Texas.
- 69.WRENN J. H. and HART G. F. (1988) - Paleogene dinoflagellate cystbiostratigraphy of Seymour Island, Antarctica. In: Geology and Paleontology of Seymour Island, Antarctic Peninsula (eds. M. Feldmann and O. Woodburnme). Mem. Geol. Soc. Am., 169: 321-447.
- 70.ZACHOS J. C., DICKENS G. R. and ZEEBE R. E. (2008) - An early Cenozoic perspective on greenhouse warming and carboncyle dynamics. Nature, 451 (7176): 279-283.
- 71.ZACHOS J., PAGANI M., SLOAN L., THOMAS E. and BILLUPS K. (2001) - Trends, rhythms, and aberrations in global climate 65 Ma to present. Science, 292 (5517): 686-693.
- 72.ZINSMEISTER W. J. (1986) - Fossil Wind fall at Antarctica's Edge. Nat. Hist., 95: 60-67.
- 73.ZINSMEISTER W. J. and de VRIES T. J. (1982) - Observation on the stratigraphy of the lower Tertiary Seymour Island Group, Seymour Island, Antarctic Peninsula. Antarctic J., 17 (5): 71-72.
- 74.YAPP C. J. (2004) - Fe(CO3)OH in goethite from a midlatitude North American oxisol: estimate of atmospheric CO2 concentration in the early Eocene "climatic optmum". Geochim. Cosmochim. Acta, 68 (5): 935-947.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS6-0035-0094