Quaternary Neogene
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Dating Methods and the Quaternary
c01.fm Page 1 Wednesday, March 23, 2005 3:21 AM 1 Dating Methods and the Quaternary Whatever withdraws us from the power of our senses; whatever makes the past, the distant or the future, predominate over the present, advances us in the dignity of thinking beings. Samuel Johnson 1.1 Introduction The Quaternary is the most recent period of the geological record. Spanning the last 2.5 million years or so of geological time1 and including the Pleistocene and Holocene epochs,2 it is often considered to be synonymous with the ‘Ice Age’. Indeed, for much of the Quaternary, the earth’s land surface has been covered by greatly expanded ice sheets and glaciers, and temperatures during these glacial periods were significantly lower than those of the present. But the Quaternary has also seen episodes, albeit much shorter in duration, of markedly warmer conditions, and in these interglacials the temperatures in the mid- and high-latitude regions may have exceeded those of the present day. Indeed, rather than being a period of unremitting cold, the hallmark of the Quaternary is the repeated oscillation of the earth’s global climate system between glacial and interglacial states. Establishing the timing of these climatic changes, and of their effects on the earth’s environment, is a key element in Quaternary research. Whether it is to date a particular climatic episode, to estimate the rate of operation of past geological or geomorphological processes, or to determine the age of an artefact or cultural assemblage, we need to be able to establish a chronology of events. -
14. Neogene and Quaternary Calcareous Nannofossil Biostratigraphy of the Walvis Ridge1
14. NEOGENE AND QUATERNARY CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY OF THE WALVIS RIDGE1 Ming-Jung Jiang, Robertson Research (U.S.) Inc., Houston, Texas and Stefan Gartner, Department of Oceanography, Texas A&M University, College Station, Texas ABSTRACT During DSDP Leg 74 in the South Atlantic, 11 holes were drilled at 5 sites (525-529) on the eastern end of Walvis Ridge. The sediments recovered range in age from late Campanian or early Maestrichtian to Holocene. This chapter deals only with the Neogene to Holocene interval. The calcareous nannofossils over this interval have been corroded as well as overgrown, but a precise biostratigraphy is possible at all sites because most of the key index species are present. INTRODUCTION CALCAREOUS NANNOFOSSIL ZONATION During DSDP Leg 74, 11 holes were drilled at 5 sites Martini's standard Tertiary and Quaternary zonation (525-529) on Walvis Ridge in the South Atlantic near (1971), which is widely used elsewhere, was the starting South Africa (Fig. 1). Sediments ranging in age from basis for the zonation described here. Because of the late Campanian or early Maestrichtian to Holocene scarcity or apparent lack of some of Martini's index fos- were recovered. This chapter deals with the calcareous sils, possibly owing to environmental exclusion of the nannofossils found in the Neogene to Holocene sedi- parent organism or to poor preservation, other species ment from these five sites. The calcareous nannofossils were selected to determine zones. Deviations from Mar- from the Paleogene and the Upper Cretaceous are docu- tinis zonation, necessary for the studied area, are dis- mented by Hélène Manivit in this same volume. -
33. Neogene and Quaternary Calcareous Nannofossils from the Blake Ridge, Sites 994, 995, and 9971
Paull, C.K., Matsumoto, R., Wallace, P.J., and Dillon, W.P. (Eds.), 2000 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 164 33. NEOGENE AND QUATERNARY CALCAREOUS NANNOFOSSILS FROM THE BLAKE RIDGE, SITES 994, 995, AND 9971 Hisatake Okada2 ABSTRACT Twenty routinely used nannofossil datums in the late Neogene and Quaternary were identified at three Blake Ridge sites drilled during Leg 164. The quantitative investigation of the nannofossil assemblages in 236 samples selected from Hole 994C provide new biostratigraphic and paleoceanographic information. Although mostly overlooked previously, Umbilicosphaera aequiscutum is an abundant component of the late Neogene flora, and its last occurrence at ~2.3 Ma is a useful new biostrati- graphic event. Small Gephyrocapsa evolved within the upper part of Subzone CN11a (~4.3 Ma), and after an initial acme, it temporarily disappeared for 400 k.y., between 2.9 and 2.5 Ma. Medium-sized Gephyrocapsa evolved in the latest Pliocene ~2.2 Ma), and after two short temporary disappearances, common specimens occurred continuously just above the Pliocene/Pleis- tocene boundary. The base of Subzone CN13b should be recognized as the beginning of the continuous occurrence of medium- sized (>4 µm) Gephyrocapsa. Stratigraphic variation in abundance of the very small placoliths and Florisphaera profunda alter- nated, indicating potential of the former as a proxy for the paleoproductivity. At this site, it is likely that upwelling took place during three time periods in the late Neogene (6.0–4.6 Ma, 2.3–2.1 Ma, and 2.0–1.8 Ma) and also in the early Pleistocene (1.4– 0.9 Ma). -
Biostratigraphy and Evolution of Miocene Discoaster Spp. from IODP Site U1338 in the Equatorial Pacific Ocean
Research article Journal of Micropalaeontology Published online December 7, 2016 https://doi.org/10.1144/jmpaleo2015-034 | Vol. 36 | 2017 | pp. 137–152 Biostratigraphy and evolution of Miocene Discoaster spp. from IODP Site U1338 in the equatorial Pacific Ocean Marina Ciummelli1*, Isabella Raffi2 & Jan Backman3 1 PetroStrat Ltd, Tan-y-Graig, Parc Caer Seion, Conwy LL32 8FA, UK 2 Dipartimento di Ingegneria e Geologia, Università ‘G. d’Annunzio’ di Chieti-Pescara, I-66013 Chieti Scalo, Italy 3 Department of Geological Sciences, Stockholm University, SE-106 91 Stockholm, Sweden * Correspondence: [email protected] Abstract: Assemblages of upper lower through upper Miocene Discoaster spp. have been quantified from Integrated Ocean Drilling Program (IODP) Site U1338 in the eastern equatorial Pacific Ocean. These assemblages can be grouped into five broad morphological categories: six-rayed with bifurcated ray tips, six-rayed with large central areas, six-rayed with pointed ray tips, five-rayed with bifurcated ray tips and five-rayed with pointed ray tips. Discoaster deflandrei dominates the assemblages prior to 15.8 Ma. The decline in abundance of D. deflandrei close to the early–middle Miocene boundary occurs together with the evolution of the D. variabilis group, including D. signus and D. exilis. Six-rayed discoasters having large central areas become a prominent member of the assemblages for a 400 ka interval in the late middle Miocene. Five- and six-rayed forms having pointed tips become prominent in the early late Miocene and show a strong antiphasing relationship with the D. variabilis group. Discoaster bellus completely dominates the Discoaster assemblages for a 400 ka interval in the middle late Miocene. -
13. Late Pliocene-Pleistocene Glaciation
13. LATE PLIOCENE - PLEISTOCENE GLACIATION W. A. Berggren, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts The discussion in this chapter is broken down into two increase in the former exceeding that of the latter; or parts: the first deals with glaciation in the North Atlantic as (v) less detritals, clay and carbonate deposited per unit time revealed in the data obtained on Leg 12; in the second part (that is, decreased sedimentation rate) with the decrease in an attempt is made to provide a chronologic framework of the latter exceeding the former. In view of the demon- Late Pliocene-Pleistocene glaciation and to correlate gla- strable increase in sedimentation rate above the preglacial/ cial/interglacial sequences as recorded in land and deep-sea glacial boundary at Sites 111, 112 and 116 due to increased sediments. amounts of detrital minerals and the fact that glacial periods in high latitudes are characterized by a carbonate GLACIATION IN THE NORTH ATLANTIC minimum (Mclntyre et al., in press) it can be seen that the One of the most significant aspects of Leg 12 was the correct explanation for the increase in natural gamma activ- various results which were obtained regarding glaciation in ity in the glacial part of the section is rather complex. Thin the North Atlantic. Glacial sediments were encountered at bands of carbonate were found at various levels intercalated all sites in the North Atlantic with the exception of Site with detrital-rich clays which indicates interglacial intervals, 117 (for the purpose of this discussion the North Atlantic so that the correct explanation probably lies with (iii) encompasses Sites 111 through 117; Sites 118 and 119 are above. -
Quaternary Calcareous Nannofossil Datums and Biochronology in the North Atlantic Ocean, IODP Site U13081 Tokiyuki Sato,2 Shun Chiyonobu,3 and David A
Channell, J.E.T., Kanamatsu, T., Sato, T., Stein, R., Alvarez Zarikian, C.A., Malone, M.J., and the Expedition 303/306 Scientists Proceedings of the Integrated Ocean Drilling Program, Volume 303/306 Data report: Quaternary calcareous nannofossil datums and biochronology in the North Atlantic Ocean, IODP Site U13081 Tokiyuki Sato,2 Shun Chiyonobu,3 and David A. Hodell4 Chapter contents Abstract Abstract . 1 We studied high-resolution Quaternary calcareous nannofossil Introduction . 1 biostratigraphy to clarify the relationship between nannofossil events and oxygen isotope stratigraphy using the continuous sed- Samples and methods. 1 iment sequence from Integrated Ocean Drilling Program Site Results . 2 U1308 in the North Atlantic Ocean. Results indicate that some Remarks on stratigraphic position of datums . 2 nannofossil events found in the section, such as the last occur- Conclusion . 3 rences of Reticulofenestra asanoi and Gephyrocapsa spp. (large), are Acknowledgments. 3 located in a different stratigraphic position compared to previous References . 3 studies. We also clarify the critical stratigraphic positions of both Figures . 5 the first occurrence of Emiliania huxleyi and the last occurrence of Table . 9 Pseudoemiliania lacunosa, which occur just below the highest peaks of each marine isotope Stage 8 and 12. Introduction Quaternary calcareous nannofossil datums and their chronostrati- graphic framework have been discussed over the last 20 y mainly based on their correlation to magnetostratigraphy (Raffi and Rio, 1979; Rio, 1982; Takayama and Sato, 1987) or to oxygen isotope stages (Thierstein et al., 1977; Wei, 1993; Raffi et al., 1993; Raffi, 2002). These studies indicate that Quaternary nannofossil datums show a small diachroneity between different latitudes. -
Applications of Calcareous Nannofossils and Stable Isotopes To
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2007 Applications of Calcareous Nannofossils and Stable Isotopes to Cenozoic Paleoceanography: Examples from the Eastern Equatorial Pacific, Western Equatorial Atlantic and Southern Indian Oceans Shijun Jiang Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] THE FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES APPLICATIONS OF CALCAREOUS NANNOFOSSILS AND STABLE ISOTOPES TO CENOZOIC PALEOCEANOGRAPHY: EXAMPLES FROM THE EASTERN EQUATORIAL PACIFIC, WESTERN EQUATORIAL ATLANTIC AND SOUTHERN INDIAN OCEANS By SHIJUN JIANG A dissertation submitted to the Department of Geological Sciences in partial fulfillment of the requirements for the degree of Doctor of Philosophy Degree Awarded: Fall Semester, 2007 The members of the Committee approve the Dissertation of Shijun Jiang defended on July 13, 2007. ____________________________________ Sherwood W. Wise, Jr. Professor Directing Dissertation ____________________________________ Richard L. Iverson Outside Committee Member ____________________________________ Anthony J. Arnold Committee Member ____________________________________ Joseph F. Donoghue Committee Member ____________________________________ Yang Wang Committee Member The Office of Graduate Studies has verified and approved the above named committee members. ii To Shuiqing and Jenny iii ACKNOWLEDGEMENTS First of all, I would like to thank my mentor Dr. Sherwood W. Wise, Jr., who constantly encouraged and supported me with his enthusiasm, reliance, guidance and, most of all, patience throughout my Ph.D adventure. He also opened a door into my knowledge of the paleo world, generously shared his time and his wealth of knowledge, patiently guided me through a western educational system totally different from my own background, and has successfully fostered my interest and enthusiasm in teaching. -
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. -
Integrated Stratigraphy and Astronomical Calibration of the Serravallian=Tortonian Boundary Section at Monte Gibliscemi (Sicily, Italy)
ELSEVIER Marine Micropaleontology 38 (2000) 181±211 www.elsevier.com/locate/marmicro Integrated stratigraphy and astronomical calibration of the Serravallian=Tortonian boundary section at Monte Gibliscemi (Sicily, Italy) F.J. Hilgen a,Ł, W. Krijgsman b,I.Raf®c,E.Turcoa, W.J. Zachariasse a a Department of Geology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands b Paleomagnetic Laboratory, Fort Hoofddijk, Budapestlaan 17, 3584 CD Utrecht, The Netherlands c Dip. di Scienze della Terra, Univ. G. D'Annunzio, via dei Vestini 31, 66013 Chieti Scalo, Italy Received 12 May 1999; revised version received 20 December 1999; accepted 26 December 1999 Abstract Results are presented of an integrated stratigraphic (calcareous plankton biostratigraphy, cyclostratigraphy and magne- tostratigraphy) study of the Serravallian=Tortonian (S=T) boundary section of Monte Gibliscemi (Sicily, Italy). Astronomi- cal calibration of the sedimentary cycles provides absolute ages for calcareous plankton bio-events in the interval between 9.8 and 12.1 Ma. The ®rst occurrence (FO) of Neogloboquadrina acostaensis, usually taken to delimit the S=T boundary, is dated astronomically at 11.781 Ma, pre-dating the migratory arrival of the species at low latitudes in the Atlantic by almost 2 million years. In contrast to delayed low-latitude arrival of N. acostaensis, Paragloborotalia mayeri shows a delayed low-latitude extinction of slightly more than 0.7 million years with respect to the Mediterranean (last occurrence (LO) at 10.49 Ma at Ceara Rise; LO at 11.205 Ma in the Mediterranean). The Discoaster hamatus FO, dated at 10.150 Ma, is clearly delayed with respect to the open ocean. -
Pleistocene Calcareous Nannofossil Biostratigraphy and Gephyrocapsid Occurrence in Site U1431D, IODP 349, South China Sea
geosciences Article Pleistocene Calcareous Nannofossil Biostratigraphy and Gephyrocapsid Occurrence in Site U1431D, IODP 349, South China Sea , Jose Dominick S. Guballa * y and Alyssa M. Peleo-Alampay Nannoworks Laboratory, National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman, Quezon City 1101, Philippines; [email protected] * Correspondence: [email protected]; Tel.: +1-28-9707-5905 Current address: Department of Earth Sciences, University of Toronto, 22 Russell Street, Toronto, y ON M5S 3B1, Canada. Received: 25 August 2020; Accepted: 23 September 2020; Published: 28 September 2020 Abstract: We reinvestigated the Pleistocene calcareous nannofossil biostratigraphy of Site U1431D (International Ocean Discovery Program (IODP) Expedition 349) in the South China Sea (SCS). Twelve calcareous nannofossil Pleistocene datums are identified in the site. The analysis confirms that the last occurrence (LO) of Calcidiscus macintyrei is below the first occurrence (FO) of large Gephyrocapsa spp. (>5.5 µm). The FO of medium Gephyrocapsa spp. (4–5.5 µm) is also identified in the samples through morphometric measurements, which was unreported in shipboard results. Magnetobiochronologic calibrations of the numerical ages of LO of Pseudoemiliania lacunosa and FO of Emiliania huxleyi are underestimated and need reassessment. Other potential markers such as a morphological turnover of circular to elliptical variants of Pseudoemiliania lacunosa and a small Gephyrocapsa acme almost synchronous with the FO of Emiliania huxleyi may offer biostratigraphic significance in the SCS. The morphologic changes in Gephyrocapsa coccoliths are also examined for the first time in Site U1431D. Placolith length and bridge angle changes are comparable with other ocean basins, suggesting that morphologic changes are most likely evolutionary novelties rather than being caused by local climate anomalies. -
An Attempt at Correlation of Main Climatostratigraphic Units of the Quaternary in the Marginal Zones of Continental Glaciations in Europe
ANNALES UNIVERSITATIS MARIAE CURIE-SKŁODOWSKA LUBLIN - POLONIA VOL.XLVIII, 14_____________________________ SECTIOB_____________________________________ 1993 Instytut Geologii Uniwersytetu Warszawskiego Leszek LINDNER, Leszek MARKS An Attempt at Correlation of Main Climatostratigraphic Units of the Quaternary in the Marginal Zones of Continental Glaciations in Europe Próba korelacji głównych jednostek klimatostratygraficznego podziału czwartorzędu w brzeżnej strefie zasięgu zlodowaceń kontynentalnych w Europie INTRODUCTION Studies of the Quaternary palaeogeographical evolution in the marginal zone of conti nental glaciations in Europe must be based on good knowledge of rhythmus of climatic changes in that time. Such changes in most cases were expressed by coolings that favou red development of 8 continental glaciations (Fig. 1) and warmings which were typical of climatic conditions during 7 interglacials, all during this part of the Quaternary that is na med the Pleistocene (Figs 2-4). From a climatostratigraphic point of view these glacia tions and interglacials, together with preceding main coolings and warmings of the Early Quaternary (Prepleistocene) as well as the following - the youngest warming of the Holo cene, are considered to be the main units of the inland Quaternary (M. D. Baraniecka 1990; L. Li n d n e r 1991b). These units are more and more frequently correlated with the 18O stages that record the main Quaternary climatic changes in deep-sea sediments (D.Q. Bowen 1989; D.Q. Bowen etal. 1989; L.Lindner 1984,1988a,b, 1991 a, b;F. Wiegank 1982; 1987; L. N. Voznyachuk 1985; V. A. Zubakov 1986, 1988, 1990; V. A. Zubakov and 1.1. Borzenkova 1990), which enables their mu tual correlations (Table 1). -
Ocean Drilling Program Scientific Results Volume
Ruddiman, W., Sarnthein M., et al., 1989 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 108 8. COMPARISON OF UPPER PLIOCENE DISCOASTER ABUNDANCE VARIATIONS FROM NORTH ATLANTIC SITES 552, 607, 658, 659, AND 662: FURTHER EVIDENCE FOR MARINE PLANKTON RESPONDING TO ORBITAL FORCING1 Alex Chepstow-Lusty,2 Jan Backman,3 and Nicholas J. Shackleton2 ABSTRACT Abundance variations of six Pliocene species of discoasters have been analyzed over the time interval from 1.89 to 2.95 Ma at five contrasting sites in the North Atlantic: Deep Sea Drilling Project Sites 552 (56°N) and 607 (41°N) and Ocean Drilling Program 658 (20°N), 659 (18°N), and 662 (1°S). A sampling interval equivalent to approximately 3 k.y. was used. Total Discoaster abundance showed a reduction with increasing latitude and from the effects of upwelling. This phenomenon is most obvious in Discoaster brouweri, the only species that survived over the entire time interval studied. Prior to 2.38 Ma, Discoaster pentaradiatus and Discoaster surculus are important components of the Discoaster assemblage: Discoaster pentaradiatus increases slightly with latitude up to 41°N, and its abundance relative to D. brouweri increases up to 56°N; D. surculus increases in abundance with latitude and with upwelling conditions relative to both D. brouweri and D. pentaradiatus and is dominant to the latter species at upwelling Site 658 and at the highest latitude sites. Discoaster asymmetricus and Discoaster tamalis appear to increase in abundance with latitude relative to D. brouweri. Many of the abundance changes observed appear to be connected with the initiation of glaciation in the North Atlantic at 2.4 Ma.