Paleobiology in the Mediterranean
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Geological-Geomorphological and Paleontological Heritage in the Algarve (Portugal) Applied to Geotourism and Geoeducation
land Article Geological-Geomorphological and Paleontological Heritage in the Algarve (Portugal) Applied to Geotourism and Geoeducation Antonio Martínez-Graña 1,* , Paulo Legoinha 2 , José Luis Goy 1, José Angel González-Delgado 1, Ildefonso Armenteros 1, Cristino Dabrio 3 and Caridad Zazo 4 1 Department of Geology, Faculty of Sciences, University of Salamanca, 37008 Salamanca, Spain; [email protected] (J.L.G.); [email protected] (J.A.G.-D.); [email protected] (I.A.) 2 GeoBioTec, Department of Earth Sciences, NOVA School of Science and Technology, Universidade NOVA de Lisboa, Caparica, 2829-516 Almada, Portugal; [email protected] 3 Department of Stratigraphy, Faculty of Geology, Complutense University of Madrid, 28040 Madrid, Spain; [email protected] 4 Department of Geology, Museo Nacional de Ciencias Naturales, 28006 Madrid, Spain; [email protected] * Correspondence: [email protected]; Tel.: +34-923294496 Abstract: A 3D virtual geological route on Digital Earth of the geological-geomorphological and paleontological heritage in the Algarve (Portugal) is presented, assessing the geological heritage of nine representative geosites. Eighteen quantitative parameters are used, weighing the scientific, didactic and cultural tourist interest of each site. A virtual route has been created in Google Earth, with overlaid georeferenced cartographies, as a field guide for students to participate and improve their learning. This free application allows loading thematic georeferenced information that has Citation: Martínez-Graña, A.; previously been evaluated by means of a series of parameters for identifying the importance and Legoinha, P.; Goy, J.L.; interest of a geosite (scientific, educational and/or tourist). The virtual route allows travelling from González-Delgado, J.A.; Armenteros, one geosite to another, interacting in real time from portable devices (e.g., smartphone and tablets), I.; Dabrio, C.; Zazo, C. -
Foucault's Darwinian Genealogy
genealogy Article Foucault’s Darwinian Genealogy Marco Solinas Political Philosophy, University of Florence and Deutsches Institut Florenz, Via dei Pecori 1, 50123 Florence, Italy; [email protected] Academic Editor: Philip Kretsedemas Received: 10 March 2017; Accepted: 16 May 2017; Published: 23 May 2017 Abstract: This paper outlines Darwin’s theory of descent with modification in order to show that it is genealogical in a narrow sense, and that from this point of view, it can be understood as one of the basic models and sources—also indirectly via Nietzsche—of Foucault’s conception of genealogy. Therefore, this essay aims to overcome the impression of a strong opposition to Darwin that arises from Foucault’s critique of the “evolutionistic” research of “origin”—understood as Ursprung and not as Entstehung. By highlighting Darwin’s interpretation of the principles of extinction, divergence of character, and of the many complex contingencies and slight modifications in the becoming of species, this essay shows how his genealogical framework demonstrates an affinity, even if only partially, with Foucault’s genealogy. Keywords: Darwin; Foucault; genealogy; natural genealogies; teleology; evolution; extinction; origin; Entstehung; rudimentary organs “Our classifications will come to be, as far as they can be so made, genealogies; and will then truly give what may be called the plan of creation. The rules for classifying will no doubt become simpler when we have a definite object in view. We possess no pedigrees or armorial bearings; and we have to discover and trace the many diverging lines of descent in our natural genealogies, by characters of any kind which have long been inherited. -
New Dinoflagellate Cyst and Acritarch Taxa from the Pliocene and Pleistocene of the Eastern North Atlantic (DSDP Site 610)
Journal of Systematic Palaeontology 6 (1): 101–117 Issued 22 February 2008 doi:10.1017/S1477201907002167 Printed in the United Kingdom C The Natural History Museum New dinoflagellate cyst and acritarch taxa from the Pliocene and Pleistocene of the eastern North Atlantic (DSDP Site 610) Stijn De Schepper∗ Cambridge Quaternary, Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, United Kingdom Martin J. Head† Department of Earth Sciences, Brock University, 500 Glenridge Avenue, St. Catharines, Ontario L2S 3A1, Canada SYNOPSIS A palynological study of Pliocene and Pleistocene deposits from DSDP Hole 610A in the eastern North Atlantic has revealed the presence of several new organic-walled dinoflagellate cyst taxa. Impagidinium cantabrigiense sp. nov. first appeared in the latest Pliocene, within an inter- val characterised by a paucity of new dinoflagellate cyst species. Operculodinium? eirikianum var. crebrum var. nov. is mostly restricted to a narrow interval near the Mammoth Subchron within the Plio- cene (Piacenzian Stage) and may be a morphological adaptation to the changing climate at that time. An unusual morphotype of Melitasphaeridium choanophorum (Deflandre & Cookson, 1955) Harland & Hill, 1979 characterised by a perforated cyst wall is also documented. In addition, the stratigraphic utility of small acritarchs in the late Cenozoic of the northern North Atlantic region is emphasised and three stratigraphically restricted acritarchs Cymatiosphaera latisepta sp. nov., Lavradosphaera crista gen. et sp. nov. -
The Gelasian Stage (Upper Pliocene): a New Unit of the Global Standard Chronostratigraphic Scale
82 by D. Rio1, R. Sprovieri2, D. Castradori3, and E. Di Stefano2 The Gelasian Stage (Upper Pliocene): A new unit of the global standard chronostratigraphic scale 1 Department of Geology, Paleontology and Geophysics , University of Padova, Italy 2 Department of Geology and Geodesy, University of Palermo, Italy 3 AGIP, Laboratori Bolgiano, via Maritano 26, 20097 San Donato M., Italy The Gelasian has been formally accepted as third (and Of course, this consideration alone does not imply that a new uppermost) subdivision of the Pliocene Series, thus rep- stage should be defined to represent the discovered gap. However, the top of the Piacenzian stratotype falls in a critical point of the evo- resenting the Upper Pliocene. The Global Standard lution of Earth climatic system (i.e. close to the final build-up of the Stratotype-section and Point for the Gelasian is located Northern Hemisphere Glaciation), which is characterized by plenty in the Monte S. Nicola section (near Gela, Sicily, Italy). of signals (magnetostratigraphic, biostratigraphic, etc; see further on) with a worldwide correlation potential. Therefore, Rio et al. (1991, 1994) argued against the practice of extending the Piacenzian Stage up to the Pliocene-Pleistocene boundary and proposed the Introduction introduction of a new stage (initially “unnamed” in Rio et al., 1991), the Gelasian, in the Global Standard Chronostratigraphic Scale. This short report announces the formal ratification of the Gelasian Stage as the uppermost subdivision of the Pliocene Series, which is now subdivided into three stages (Lower, Middle, and Upper). Fur- The Gelasian Stage thermore, the Global Standard Stratotype-section and Point (GSSP) of the Gelasian is briefly presented and discussed. -
Epilogue: Pattern Cladistics from Goethe to Brady
Epilogue: Pattern Cladistics From Goethe to Brady Most, if not all, ideas in science are recycled, rediscovered, or rehashed, either sur- reptitiously, through rereading and rediscovering old works, or simply (commonly?) through lack of knowledge of past achievements. The idea of transformation—that things might change, transform, convert into other things—for instance, has been proposed many times, by both evolutionists and non-evolutionists alike. Yet the notion of transformation is really a myth, a story which many scientists embrace, a story that tells of living things transforming into other living things, with their role to interpret its meaning and mechanism: The fall of Paradise to the untamed wild, the tamed landscape to the Biblical flood, the reigns of monarchs, a kingdom to a republic and the pastoral to the industrial—of transformations there are plenty. A deep desire to uncover what mechanism(s) lie behind these transformations has provided many explanations, from the acquisition of sin after the fall from grace, to God’s will, to progress, however construed. The belief that every transformation neatly fits a law or model by which nature abides has shaped our way of thinking. Yet concomitant with such thoughts is the recognition that Nature is complex, and that Nature’s complexity obeys no single law or theory that places it neatly into a box. For every law and theory, we are told, there are exceptions, which are given ad hoc explanations. Man may have toiled the soil to shape nature into his or her image of Eden, but complexity does not fit any man-made law. -
GEOLOGIC TIME SCALE V
GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE -
Paleogeographic Maps Earth History
History of the Earth Age AGE Eon Era Period Period Epoch Stage Paleogeographic Maps Earth History (Ma) Era (Ma) Holocene Neogene Quaternary* Pleistocene Calabrian/Gelasian Piacenzian 2.6 Cenozoic Pliocene Zanclean Paleogene Messinian 5.3 L Tortonian 100 Cretaceous Serravallian Miocene M Langhian E Burdigalian Jurassic Neogene Aquitanian 200 23 L Chattian Triassic Oligocene E Rupelian Permian 34 Early Neogene 300 L Priabonian Bartonian Carboniferous Cenozoic M Eocene Lutetian 400 Phanerozoic Devonian E Ypresian Silurian Paleogene L Thanetian 56 PaleozoicOrdovician Mesozoic Paleocene M Selandian 500 E Danian Cambrian 66 Maastrichtian Ediacaran 600 Campanian Late Santonian 700 Coniacian Turonian Cenomanian Late Cretaceous 100 800 Cryogenian Albian 900 Neoproterozoic Tonian Cretaceous Aptian Early 1000 Barremian Hauterivian Valanginian 1100 Stenian Berriasian 146 Tithonian Early Cretaceous 1200 Late Kimmeridgian Oxfordian 161 Callovian Mesozoic 1300 Ectasian Bathonian Middle Bajocian Aalenian 176 1400 Toarcian Jurassic Mesoproterozoic Early Pliensbachian 1500 Sinemurian Hettangian Calymmian 200 Rhaetian 1600 Proterozoic Norian Late 1700 Statherian Carnian 228 1800 Ladinian Late Triassic Triassic Middle Anisian 1900 245 Olenekian Orosirian Early Induan Changhsingian 251 2000 Lopingian Wuchiapingian 260 Capitanian Guadalupian Wordian/Roadian 2100 271 Kungurian Paleoproterozoic Rhyacian Artinskian 2200 Permian Cisuralian Sakmarian Middle Permian 2300 Asselian 299 Late Gzhelian Kasimovian 2400 Siderian Middle Moscovian Penn- sylvanian Early Bashkirian -
Ratification of Subseries/Subepochs As Formal Rank/Units in International Chronostratigraphy
Communication of IUGS Geological Standards 1 by Marie-Pierre Aubry1, Werner E. Piller2*, Philip L. Gibbard 3, David A. T. Harper4, and Stanley C. Finney5 Ratification of subseries/subepochs as formal rank/units in international chronostratigraphy 1 Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08873, USA 2 Institute of Earth Sciences, University of Graz, NAWI Graz Geocenter, Heinrichstrasse 26, 8010 Graz, Austria; *Corresponding author: E-mail: [email protected] 3 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge CB2 1ER, UK 4 Department of Earth Sciences, Durham University, Durham DH1 3LE, UK 5 Department of Geological Sciences, California State University, Long Beach, USA (Received: May 27, 2021; Revised accepted: July 8, 2021) https://doi.org/10.18814/epiiugs/2021/021016 The IUGS Executive Committee has voted unanimously should they remain informal subdivisions of series and epochs in a to ratify the proposal for formal adoption of the five-tiered hierarchy? This dilemma was at the heart of the conflicting posi- chronostratigraphical/geochronological unit divisions tions expressed in Head et al. (2017) and Pearson et al. (2017). A subseries/subepoch within the International Stratigraphic temporary resolution to the situation was recommended, so that sub- Guide as approved by the International Commission on commissions had the freedom to choose between formal and infor- Stratigraphy and forwarded to the IUGS EC on 24 March mal status based on individual preference (Finney and Bown, 2017). 2021**. The subseries/subepochs are now incorporated This led to glaring inconsistency in Cenozoic chronostratigraphy, in that the Subcommission on Quaternary Stratigraphy (SQS) adopted a in a six-tiered chronostratigraphic hierarchy of units that formal status for subseries whereas the subcommissions on Neogene are formally defined by a designated GSSP (Global Stage and Paleogene Stratigraphy (SNS and ISPS) continued to use sub- Stratotype and Point) at the base of designated type stages. -
INTERNATIONAL CHRONOSTRATIGRAPHIC CHART International Commission on Stratigraphy V 2020/03
INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2020/03 numerical numerical numerical numerical Series / Epoch Stage / Age Series / Epoch Stage / Age Series / Epoch Stage / Age GSSP GSSP GSSP GSSP EonothemErathem / Eon System / Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) Eonothem / EonErathem / Era System / Period GSSA age (Ma) present ~ 145.0 358.9 ±0.4 541.0 ±1.0 U/L Meghalayan 0.0042 Holocene M Northgrippian 0.0082 Tithonian Ediacaran L/E Greenlandian 0.0117 152.1 ±0.9 ~ 635 U/L Upper Famennian Neo- 0.129 Upper Kimmeridgian Cryogenian M Chibanian 157.3 ±1.0 Upper proterozoic ~ 720 0.774 372.2 ±1.6 Pleistocene Calabrian Oxfordian Tonian 1.80 163.5 ±1.0 Frasnian 1000 L/E Callovian Quaternary 166.1 ±1.2 Gelasian 2.58 382.7 ±1.6 Stenian Bathonian 168.3 ±1.3 Piacenzian Middle Bajocian Givetian 1200 Pliocene 3.600 170.3 ±1.4 387.7 ±0.8 Meso- Zanclean Aalenian Middle proterozoic Ectasian 5.333 174.1 ±1.0 Eifelian 1400 Messinian Jurassic 393.3 ±1.2 Calymmian 7.246 Toarcian Devonian Tortonian 182.7 ±0.7 Emsian 1600 11.63 Pliensbachian Statherian Lower 407.6 ±2.6 Serravallian 13.82 190.8 ±1.0 Lower 1800 Miocene Pragian 410.8 ±2.8 Proterozoic Neogene Sinemurian Langhian 15.97 Orosirian 199.3 ±0.3 Lochkovian Paleo- Burdigalian Hettangian proterozoic 2050 20.44 201.3 ±0.2 419.2 ±3.2 Rhyacian Aquitanian Rhaetian Pridoli 23.03 ~ 208.5 423.0 ±2.3 2300 Ludfordian 425.6 ±0.9 Siderian Mesozoic Cenozoic Chattian Ludlow -
Late Pliocene and Pleistocene Biostratigraphy of the Nordic Atlantic Region
Newsletters on Stratigraphy © Gebrüder Borntraeger 2008 Vol. 43/1: 33–48, June 2008 Late Pliocene and Pleistocene biostratigraphy of the Nordic Atlantic region Erik D. Anthonissen1 With 3 figures and 1 appendix Abstract. The lack of primary and secondary GSSP correlative markers in Plio-Pleistocene deposits of the North Sea, Nordic seas and northern North Atlantic creates a challenge for the biostratigrapher. This study highlights the closest biostratigraphic approximations in this region to the standard chronostratigraphic boundaries of the Gelasian Stage and Lower, Middle and Upper Pleistocene. Via correlations to key Ocean Drilling studies and unambiguous magnetostratigraphies in the region, the age of shallower deposits of the North Sea has been better constrained. The closest biostratigraphic approximations to these chronostrati- graphic boundaries in the region are presented, together with a framework of calibrated events according to sub-basin. The best approximating boundary events at any given location in this region depends upon both the paleoceanographic and paleobathymetric settings. In the Nordic Atlantic region only three GSSP correl- ative marker events have been identified in the 15 Ocean Drilling Program sites discussed. At lower neritic to bathyal water depths, the first common occurrence of Neogloboquadrina pachyderma (sinistrally-coiled morphotype) allows for direct correlation with the base Pleistocene GSSP in Italy. The occurrence of the ben- thic foraminifer Cibicides grossus appears to have been bathymetrically controlled, with a youngest strati- graphic occurrence at upper bathyal depths. At lower neritic depths in the central and northern North Sea the last occurrence of C. grossus coincides with the base of the Pleistocene. Diachroneity of a number of Nordic high-latitude bioevents may be primarily due to differences in surface water masses and paleobathymetry. -
The PRISM4 (Mid-Piacenzian) Paleoenvironmental Reconstruction
Clim. Past, 12, 1519–1538, 2016 www.clim-past.net/12/1519/2016/ doi:10.5194/cp-12-1519-2016 © Author(s) 2016. CC Attribution 3.0 License. The PRISM4 (mid-Piacenzian) paleoenvironmental reconstruction Harry Dowsett1, Aisling Dolan2, David Rowley3, Robert Moucha4, Alessandro M. Forte5,6, Jerry X. Mitrovica7, Matthew Pound8, Ulrich Salzmann8, Marci Robinson1, Mark Chandler9,10, Kevin Foley1, and Alan Haywood2 1Eastern Geology and Paleoclimate Science Center, United States Geological Survey, Reston, VA 20192, USA 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK 3Department of the Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA 4Department of Earth Sciences, Syracuse University, Syracuse, NY 13244, USA 5Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA 6GEOTOP, Université du Québec à Montréal, Montréal QC, H3C 3P8, Canada 7Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA 8Department of Geography, Faculty of Engineering and Environment, Northumbria University, Newcastle upon Tyne NE1 8ST, UK 9Center for Climate Systems Research at Columbia University, New York, NY, USA 10NASA Goddard Institute for Space Studies, New York, NY, USA Correspondence to: Harry Dowsett ([email protected]) Received: 16 March 2016 – Published in Clim. Past Discuss.: 21 March 2016 Revised: 22 June 2016 – Accepted: 23 June 2016 – Published: 13 July 2016 Abstract. The mid-Piacenzian is known as a period of rel- 1 Introduction ative warmth when compared to the present day. A compre- hensive understanding of conditions during the Piacenzian The Pliocene, specifically the mid-Piacenzian (3.264 to serves as both a conceptual model and a source for boundary 3.025 Ma), has been a focus of synoptic paleoclimate re- conditions as well as means of verification of global climate search for the past 25 years. -
HSNS4801 03 Sepkoski 56..109
DAVID SEPKOSKI* AND MARCO TAMBORINI§ ‘‘An Image of Science’’: Cameralism, Statistics, Downloaded from http://online.ucpress.edu/hsns/article-pdf/48/1/56/377855/hsns_2018_48_1_56.pdf by Max Planck Institute for the History of Science user on 15 June 2021 and the Visual Language of Natural History in the Nineteenth Century ABSTRACT This paper traces the emergence of a new visual language for statistical paleontology in the early nineteenth century as part of a broader project to uncover a deep genealogy of modern practices in data visualization. In the first decades of the nineteenth century, natural historians had amassed large quantities of taxonomic data, but lacked quantitative and visual methods to produce and communicate knowledge derived from their data collections. As our ‘‘main witness’’ (in Ian Hacking’s sense), we call on the German paleontologist H. G. Bronn—one of the earliest pro- ponents of a ‘‘data-driven’’ approach to statistical natural history—to highlight two unexpected sources of a transformative visual idiom introduced at the time: so-called spindle diagrams representing historical patterns in taxonomic diversity. The first source—which informed Bronn’s general statistical approach to fossil data—was the bureaucratic science of cameralism, in which Bronn was steeped as a student and professor at the University of Heidelberg. The second was an earlier tradition of historical visualization popularized by Joseph Priestley and others, which represented time—or the ‘‘timeline’’—as measured graphical space on the horizontal axis of a chart. In combining the tabular statistical approach of Heidelberg cameralism and the historical timeline, Bronn contributed to the emergence of a powerful new visual language for producing and communicating aggregative statistical generalizations.