WESTERN PACIFIC EARTH SCIENCES, Vol.7, P.1-20, December, (Geological Time Scale GTS) ( ) (ISC) (INQUA) Quaternary

Similar documents
International Commission on Stratigraphy Subcommission on Quaternary Stratigraphy

INTERNATIONAL COMMISSION ON STRATIGRAPHY. To: IUGS Executive Regarding: Definition and Rank of Quaternary. Dear IUGS, Summary of Recommendations:

Quaternary Geology For Geology BSc. Students, Tanta University, Ali Soliman 1

Definition and geochronologic/chronostratigraphic rank of the term Quaternary

Hierarchical subdivision of the Cenozoic Era: A venerable solution, and a critique of current proposals

Minutes of the meeting of the Geological Society Stratigraphy Commission, 18 th May 2016, at Burlington House, London, in the Council Room.

Chronostratigraphy. References. Introduction

A case for formalizing subseries (subepochs) of the Cenozoic Era (a)

What can lithostratigraphy do for you?

Stratigraphy. Lecture 3

Quaternaire Éditeur : Association Française pour l Étude du Quaternaire

The Neogene and Quaternary: chronostratigraphic compromise or non-overlapping magisteria?

Global chronostratigraphical correlation table for the last 2.7 million years

Chronostratigraphy and geochronology: A proposed realignment

Cenozoic chronostratigraphic terminology: In defense of formal subseries

The GSSP Concept Report of the International Commission on Stratigraphy Workshop, Prague, May 31 June 3, 2010.

Quaternary International

By R. M. Carter, S. T. Abbott and T. R. Naish School of Earth Sciences, James Cook University, Townsville, Australia

THE COMMISSION FOR THE GEOLOGICAL MAP OF THE WORLD

EARTH SCIENCE WEEK SCHOOLS EVENT THE ANTHROPOCENE

Minutes of the meeting of the Geological Society Stratigraphy Commission, 8 th March 2017, at Burlington House, London, in the Council Room.

GY 111: Physical Geology

North American Commission on Stratigraphic Nomenclature

Norwegian Interactive Offshore Stratigraphic Lexicon: Cretaceous Mike Charnock StatoilHydro Geo Workshop Meeting NPD 16 October 2009

The term 'Anthropocene' in the context of formal geological classification

Vrica-Crotone and Montalbano Jonico sections: A potential unit-stratotype of the Calabrian Stage

Age of Earth/Geologic Time. Vocabulary

International Subcommission on Stratigraphic Classification ISSC

A Joint European GIS Under Construction: The 1:5 Million International Geological Map of Europe and Adjacent Areas (IGME 5000)

Ch. 19 The Neogene World

Geologic Trips San Francisco and the Bay Area

Geological Time Scale UG Hons.1 st Year) DR. CHANDAN SURABHI DAS ASST. PROF. IN GEOGRAPHY BARASAT GOVT. COLLEGE

QUATERNARY AUSTRALASIA. Quaternary, quo vadis? Proposed Neogenisation of the Quaternary, and Quaternarists response

TIME LINE OF LIFE. Strip for Clock of Eras representing the circumference. 1. Review the eras represented on the Clock of Eras:

Efficient Chrono-Stratigraphic Database Structure in GIS

Middle Eocene western north Atlantic biostratigraphy and environmental conditions

Absolute Time. Part 8 Geochronology and the Time Scale

Chapter 3 Time and Geology

Mountains Rise and Valleys Sink: Geology Demonstrates Psalm 104:8

Science 20. Unit C: The Changing Earth. Assignment Booklet C3

Chapter 3 Time and Geology

Deep Time and the Geologic Time Scale

Terminology of geological time: Establishment of a community standard

The Lithosphere and the Tectonic System. The Structure of the Earth. Temperature 3000º ºC. Mantle

Stratigraphy. The part of geology that deals with the formation, composition, sequence, and correlation of rocks, especially stratified rocks

Lab 2 Geological Time and Fossil Samples

FIGURE L5.1 Horizontal rock layers are easy to see (a) at the Grand Canyon in Arizona and (b) near Khasab in Oman (a country in the Middle East)

Figs 1-5. Prepared on behalf of the Subcommission on Quaternary Stratigraphy (SQS) by Maria Bianca Cita. Foreword

Page 143: Geologic Time

Geologica Acta: an international earth science journal ISSN: Universitat de Barcelona España

How do we learn about ancient life? Fossil- a trace or imprint of a living thing that is preserved by geological processes.

SAMPLE QUESTIONS FOR GEOLOGY 103, TEST 1

EARTH S HISTORY. What is Geology? logy: science. Geology is the scientific study of the Earth, including its:

Curriculum Vitae. Mob No ,

The terrestrial rock record

Paleoceanography II Telluric Effects on Oceanography

GEL 113 Historical Geology

A formal model for the geologic time scale and global stratotype section and point, compatible with geospatial information transfer standards

Stratigraphy and Geologic Time. How old are the rocks?

IUGS. A Global Player in Geoscience. International Union of Geological Sciences

46. DATA REPORT: LATE PLIOCENE DISCOASTER ABUNDANCES FROM HOLE 806C 1

APPLICATION OF DYNAMIC PROGRAMMING TO THE DATING OF A LOESS-PALEOSOL SEQUENCE

GEO4240: 3D Seismic Interpretation Project

History, philosophy, and application of the Global Stratotype Section and Point (GSSP)

Geologic Time. The Cenozoic Era. 7. Mammals evolved after dinosaurs became extinct.

WESTERN STATES SEISMIC POLICY COUNCIL POLICY RECOMMENDATION Definitions of Recency of Surface Faulting for the Basin and Range Province

The Geology of Stratigraphic Sequences

IODP Proposal Cover Sheet 914 -

What s new in TS-Creator version 5.4 Released 1 June 2012

Biostratigraphic and Lithostratigraphic Correlation of Sedimentary Strata in the Atlantic Coastal Plain

Accuracy of dating methods utilised

Neogene Uplift of The Barents Sea

PALEOCEANOGRAPHY, VOL. 3, NO. 5, PAGES , OCTOBER College of Oceanography Oregon State University, Corvallis

GSA DATA REPOSITORY

Variations in the Earth's Orbit: Pacemaker of the Ice Ages

QUATERNARY AND GLACIAL GEOLOGY

Geologic Time. Geologic Events

Status of Living and Extinct Taxa. Mammals Amphibians Birds. Nearly 1/3 (31%) is globally threatened or extinct. DRAFT

Age of the Tananwan Formation in Northern Taiwan: A Reexamination of the Magnetostratigraphy and Calcareous Nannofossil Biostratigraphy

Geology Merit Badge Workbook

EGAS. Ministry of Petroleum

Listing of Sessions per INQUA Commission

The Humanized Earth System

Table DR1. Radioisotope ages used to establish astrochronology of the Piobbico core. (1993)

Search and Discovery Article # (2015) Posted April 20, 2015

Frome uranium province, South Australia: Systems analysis and potential for major basin-hosted uranium deposits

A lithostratigraphical framework for onshore Quaternary and Neogene (Tertiary) superficial deposits of Great Britain and the Isle of Man

Biology. Slide 1 of 40. End Show. Copyright Pearson Prentice Hall

International Commission on Stratigraphy (ICS)

IUGS. A Global Player in Earth Science. International Union of Geological Sciences

Case Study of the Structural and Depositional-Evolution Interpretation from Seismic Data*

Minutes of the meeting of the Geological Society Stratigraphy Commission, 23 rd November 2016, at Burlington House, London, in the Arthur Holmes Room.

1 Introduction f. m. gradstein

} Institute of Earth Sciences, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands

EGAS. Ministry of Petroleum

Plio-Pleistocene Geology

Hosgri-San Simeon Fault Zone Geologic Slip Rate

Loess and dust. Jonathan A. Holmes Environmental Change Research Centre

Palaeomagnetic Study on a Granitic Rock Mass with Normal and Reverse Natural Remanent Magnetization

Science Data Representation Questions: Strategies and Sample Questions

Transcription:

( ) 1-20 200 12 WESTERN PACIFIC EARTH SCIENCES, Vol., P.1-20, December, 200 2004 (Geological Time Scale GTS) ( ) (ISC) (INQUA) (1) (2)ICS (3) (4) Clague(2005) Pillans(2004) (1) (2) (Period/System) (3) Pleistocene (4)Pleistocene (1.81 Ma) Gelasian (2.6 Ma) 1. weiky@ntu.edu.tw 1

2 Western Pacific Earth Sciences, Vol. 1 ( Period) 2004 (Geological Time Scale GTS)(Gradstein et al., 2004a,b) Period Sub-Era Period System 196 (International Stratigraphic Guide)(Hedberg, 196) ( ) 2 ( ) Gibbard et al.(2005) Aubry et al.(2005) Arduino 160 Denoyers 1829 Primary-Secondary-Tertiary

Wei: status and boundary 3 Table 1. Chinese terminologies of chronostratigraphic and geochronologic units used in this article and their corresponding English terms. 180 Pleistocene (Lyell) 185 Newer Pliocene( Pleistocene) Diluvium Tertiary Newer Pliocene Pleistocene (1) Pleistocene (2) Pleistocene (Onset of Northern Hemisphere Glaciation) (Pleistocene) (Homo) G. S. Gruner 1806 Anthropogene( ) (, 2005) 1948 (International Geology Congress, IGC)

4 Western Pacific Earth Sciences, Vol. Pleistocene Calabrian Stage ( ) 1992 (International Association INQUA) Pleistocene Vrica 1.64 Ma 1.81 Ma(Lourens et al., 1996) 1.81 Ma Shackleton(199) Pleistocene 103 (MIS103) 2.4 Ma 2.6 Ma 1996 (International Commission on Stratigraphy ICS) Gela Monte San Nicola Gelasian Stage GSSP 2.588 Ma MIS103 2.6 Ma (Rio et al., 1998) INQUA 1998 Pleistocene GSSP(Global Standard Section and Point golden spike) Gelasian Stage ICS (moratorium) 2008 ICS 2004 INQUA 2008 3 2004 (Geological Time Scale GTS)

Wei: status and boundary 5 GTS (lithologic stratigraphy) (chronostratigraphy) (geochronology) GTS Gradstein 2004 (Gradstein et al., 2004a,b) GTS Neogene (Period/System) Miocene Pliocene Pleistocene Holocene( )(, 2005) (Paleogene Period) (Neogene Period)(, 2001) ( Pillans, 2006) Figure 1. Four schemes dealing with the status and boundaries of the proposed by various geological organizations in recent years (extracted from Pillans, 2006).

6 Western Pacific Earth Sciences, Vol. GTS2004 Gradstein ( Gradstein and Ogg, 2002 Ogg, 2004) Primary Secondary Tertiary (antiquated) Gradstein (ICS) GTS2004 ICS GTS2004 250 Tertiary (Giles, 2005) (International Union of Geological Sciences IUGS) Episodes INQUA GTS2004 (Clague, 2004) (ICS-INQUA Task Group) (Gradstein and Clague, 2005) 2005 9 Leuven 2006 3 INQUA (INQUA Executive) ICS (Gradstein et al., 200) 4 GTS1982 GTS1989 (Sub-Erathem) Pleistocene ( Pleistocene Series Holocene Series) 1994 (International Stratigraphic Guide)(Salvador, 1994) System GTS2004 Tertiary ( ) 2004 INQUA INQUA ICS ICS (Gibbard, 2006) ICS 2005 9 Leuven ( )(Clague, 2005) (1)

Wei: status and boundary Sub-Erathem/Sub-Era (2) Sub-Erathem Gelasian (2.6-1.8 Ma) Gelasian Pliocene Series (3) Sub-Erathem Neogene System ( Tertiary) ( Gelasian Neogene ) (1) Sub-Era (2.6 Ma ) Neogene System (23.03 Ma ) (2) Neogene System Miocene Pliocene Pleistocene Holocene Series (Sub-Era) Neogene System ( Pliocene Pleistocene Holocene) (3) Tertiary Pliocene Stages GTS 3 Ahmedahad ICS Gradstein INQUA 2006 INQUA 2006 (1) Neogene Paleogene (2) ( ) ( ) ( ) (3) Gelasian ( Gelasian ) (Gelasian ) (Lower, Middle and Upper Subseries)( ) INQUA 2006 (1) (2) (Lower Subseries) Geleasian Lower

8 Western Pacific Earth Sciences, Vol. Subseries (3) Pleistocene Pliocene (PP boundary) Gelasian GTS INQUA Pliocene ICS Gradstein 2006 20 INQUA (Gradstein et al., 200) (1) IGC 1948 Neogene 1948 (GSSP) (2) 1985 ICS INQUA Pleistocene (3) IUGS 1991 Paleogene GSSP 1996 Neogene GSSP Tertiary 20 IGC Tertiary Cenozoic (synonym) IGC Tertiary 1985 IGC INQUA Pleistocene ( Pleistocene ) (4) ICS INQUA MIS103 (2.59 Ma)( Shackleton 199 ) (2. Ma) C2r ( Matuyama Gauss 2.58 Ma) Gelasian ICS INQUA Gelasian (5) ICS IUGS IGC (6) (a) (b)pleistocene Gelasian

Wei: status and boundary 9 () ICS (Sub-Era) (Period) Pleistocene Gelasian Pleistocene IGC 1948 1998 INQUA IUGS 1948 IGC (8) Pleistocene Series GSSP(1985 ) ( Pt1 CN13b RN13 NALMA Irvingtonian ) ( C1r ) Gelasian (Matuyama) 5 INQUA 2005 INQUA (see the e-mail sent by late Nick Shackleton to Dr. Gradstein on 12 May, 2005, as cited in Gradstein. 200, p.130) (1) GTS (2) Tertiary (Sub-Era) Paleogene Neogene (3) 2.6 Ma INQUA 2006 3 Ahmedahad Paleogene Neogene INQUA 200 8 (Cairns) Alan Chivas ICS 2008 GTS 2008 8 (IGC) INQUA 2008 IUGS ICS

10 Western Pacific Earth Sciences, Vol. Pleistocene Pleistocene Gelasian Gelasian INQUA INQUA 2006 INQUA (International Council of Scientific Unions ICSU) (International Union of Geological Sciences, IUGS) ICS IUGS INQUA ICS IUGS IUGS IGC 6 GTS2004 Tertiary ( ) Walsh(2006) ICS (Guideline) C Tertiary (1)A (Pillans and Naish, 2004) GTS2004 Neogene Period Sub-Period INQUA (Pillans INQUA Stratigraphy and Chronology Commission ) GTS2004 Hornes (Vienna Basin) Neogene Neogene Quateranry Paleogene( Bowen and Gibbard, 200, p.3-4 Walsh, 2006, p.215)

Wei: status and boundary 11 A Pleistocene ICS Leuven 2005 INQUA ( ) A ICS Sub-Period GTS2004 (2)B (Aubry et al., 2005) Tertiary Sub-Era Neogene Paleogene Holocene Pleistocene Tertiary- Sub-Eras Paleogene-Neogene Periods Tertiary- Sub-Era ( Walsh, 2006) Figure 2. Three recently proposed schemes on the status and boundaries of the (from Walsh, 2006).

12 Western Pacific Earth Sciences, Vol. Neogene Period Sub- Era ICS Leuven 2005 ( ) Aubry et al.(2005) B W.A. Berggren Paleogene-Neogene Tertiary- GTS 2004 Aubry et al.(2005) (3)C (Gibbard et al., 2005) Neogene Paleogene (Period) Pleistocene Gelasian Age INQUA INQUA 2006 ( ) (1) Pleistocene Epoch Early Pleistocene earliest Gelasian Age Pleistocene Early Middle Late (2) (Tertiary) ( ) ( ).1 (GTS) (hierarchy) (hierarchical classification) ( Leuven 2005 Neogene System Sub-Erathem Tertiary Sub-Erathem ) )

Wei: status and boundary 13 Leuven(2005)( ) Aubry et al.(2005)( B) (1) Sub-Era Neogene Period Neogene Period Sub-Era Neogene Period (2) Pliocene Tertiary ( Pliocene) (subordinate).2 ISC (Remane et al., 1996, p.8) The Global Chronostratigraphic Scale must, however, comprise strictly contiguous units, without overlaps and with no gaps between them. ( ) ( Jurassic Cretaceous ) Aubry et al.(2005)( B) Gelasian Pliocene Epoch Sub-Era Tertiary Sub-Era (topological) Pliocene Tertiary Pliocene Sub-Era.3 (Simpson's rule) INQUA 2006( ) Pleistocene Series subseries stage

14 Western Pacific Earth Sciences, Vol. Pleistocene (Subseries vs. Stage).4 (convention of conterminosity) ISC (Remane et al., 1996, p.8) The lower boundaries of chronostratigraphic units of higher rank (series, systems etc.) are automatically defined by the base of their lowermost stage. ( ) (convention of conterminosity) (Harland et al., 1990, p.20) Pleistocene INQUA Pleistocene Pliocene Gelasian Leuven(2005)( ) Pillans and Naish(2004)( A) Aubry et al.(2005)( B) (1) INQUA2005 Sub-Era Sub-Era ( Sub-Era) (Tertiary Sub-Era) (Neogene) (2) INQUA ( ) Gelasian Gelasian INQUA2006 INQUA ICS Sub Era ICS (1) Pleistocene Gelasian (2)

Wei: status and boundary 15 Pleistocene INQUA (1) Sub Era (2) Pleistocene Gelasian Pleistocene ( ) Pleistocene Pleistocene (a) (b) (c) INQUA 2.6Ma ( Homo habilis H. rudolfensis) Neogene(Pliocene) 8 (1) (2) (Period) (3)Pleistocene Gelasian (4) Pleistocene Clague(2005) 3 (status quo) ( Salvador, 1994) Tertiary ( Tertiary System Paleogene System Neogene System ) Pillans(2004) present (1)Tertiary (2)

16 Western Pacific Earth Sciences, Vol. INQUA Paleogene Neogene ( ) (1)ISC (2)INQUA Pliocene Gelasian ICS ( Pillans and Naish, 2004) Figure 3. The recommended version adopted from Pillans and Naish (2004).

Wei: status and boundary 1 NSC96-252-M-002-012-PAE 59 2001 IX 2005 25 6 60-65 (2005) 5 4 1-9 Aubry, M.P., Berggren, W.A., van Couvering, J., McGowran, B., Pillans, B. and Hilgen, F. (2005) : status, ranks, definition, survival: Episodes, 28, 118-120. Bowen, D.Q. and Gibbard, P.L. (200) The is here to stay: J. Sci., 22 (1), 3-8. Clague, J. (2004) INQUA, IUGS, and the 32 nd International Geological Congress: Quat. Perspective, 14(2), 8-88. Clague, J. (2005) Status of the : Quat. Sci.Reviews, 24, 2424-2425. Gibbard, P.L. (2006) International Commission on Stratigraphy Workshop, Leuven, Belgium, 1-5 September 2005: Quat. Int., 14, 11-119. Gibbard, P.L., Smith, A.G., Zalasiewicz, J.A., Barry, T.L., Cantrill, D., Coe, A.L., Cope, J.C. W., Gale, A.S., Gregory, F.J., Powell, J.H., Rawson, P.F., Stone, P. and Waters, C.N. (2005) What status for the?: Boreas, 34, 1-6. Giles, J. (2005) Geologists call time on dating dispute: Nature, 435, 865. Gradstein, F.M. and Clague, J. (2005) Announcement of the ICS-INQUA joint task force on the : Quat. Int., 129, 91. Gradstein, F.M., Finney, S. and Ogg, J. (200) Current IUGS-IGC decision on and

18 Western Pacific Earth Sciences, Vol. on Pleistocene: Quat. Int., 160, 129-131. Gradstein, F.M. and Ogg, J.G. (2002) Future directions in stratigraphy: Episodes, 25, 203-208. Gradstein, F.M., Ogg. J.G., Smith, A.G., Bleeker, W. and Lourens, L.J. (2004a) A new Geologic Time Scale, with special reference to Precambrian and Neogene: Episodes, 2, 83-100. Gradstein, F.M., Ogg, J.G., Smith, A.G. and others. (2004b) A Geologic Time Scale 2004, Cambridge University Press, Cambridge, UK, 589 p. Harland, W.B., Armstrong, R.L., Cox, A.V., Craig, L.E., Smith, A.G. and Smith, D.G. (1990) A Geologic Time Scale 1989, Cambridge University Press, Cambridge, UK, 263 p. Hedberg, H.D. (196) International Stratigraphic Guide. A Guide to Stratigraphic Classification, Terminology and Procedure. (International Subcommittee on Stratigraphic Classification, IUGS Commission on Stratigraphy), John Wiley & Sons, New York, 200 p. Lourens, L.J., Antonarakou, A., Hilgen, F.J., Van Hoof, A.A.M., Vergnaud-Grazzini, C. and Zachariasse, W.J. (1996) Evaluation of the Plio-Pleistocene astronomical timescale: Paleoceanography, 11(4), 391-413. Ogg, J.G. (2004) Introduction to concepts and proposed standardization of the term "": Episodes, 2, 125-126. Pillans, B. (2004) Proposal to redefine the : Episodes, 2,12-12. Pillans, B. (2006) Defining the : where do we go from here?: Australia, 24(1), 2-4. Pillans, B. and Naish, T. (2004) Defining the : Quat. Sci.Reviews, 23, 221-2282. Remane, J., Bassett, M.G., Cowie, J.W., Gohrbandt, K.H., Lane, H.R., Michelson, O. and Naiwen, W. (1996) Revised guidelines for the establishment of global chronostratigraphic standards by the International Commission on Stratigraphy (ICS): Episodes, 19, -81. Rio, D., Sprovieri, R., Castradori, D., Di Stefano, E. (1998) The Gelasian Stage Upper Pliocene: a new unit of the global standard chronostratigraphic scale: Episodes, 21, 82-8. Salvador, A. (Ed.) (1994) International Stratigraphic Guide, 2 nd ed. International Union of Geological Sciences and The Geological Society of America, Trondheim, Norway, and Boulder, CO. 214 p. Shackleton, N.J. (199) The deep sea record and the Pliocene-Pleistocene boundary: Quat. Int., 40, 33-35. Walsh, S.L. (2006) Hierarchical subdivisions of the Cenozoic Era: a venerable solution, and a critique of current proposals: Earth Science Reviews, 8, 20-23.

Wei: status and boundary 19 ON THE SURVIVAL, RANK AND BOUNDARY OF THE QUATERNARY KUO-YEN WEI 1 1. Department of Geosciences, National Taiwan University, Taipei, Taiwan, R.O.C. ABSTRACT The omission of the from the newly published Geologic Time Scale 2004 has caused hot debates on the survival, rank, definition and boundary of the among geoscientists and between geologic organizations, such as the International Commission on Stratigraphy (ICS) and International Union for Research (INQUA). This article comments on several proposals and options appeared in recent years. Based on consideration of (1) general rules of ranked hierarchy, (2) ICS guideline of no overlapping or gaps between units, (3) Simpson's rule, and (4) convention of conterminosity, the author suggests to adopt the option 3rd of the status quo version in Clague (2005) (same as the "present version" in Pillans, 2004), namely, (1) keeping the as a formal ranked chronostratigraphic unit, (2) retaining the rank as the Period/System, (3) coupling the lower boundaries of the and the Pleistocene and (4) retaining the current Pleistocene GSSP at 1.81 Ma without extending the lower Pleistocene boundary to the base of the Gelasian (2.6 Ma). Key words:, Pleistocene, Neogene, stratigraphy, chronostratigraphy, geologic time scale 1. Kuo-Yen Wei, e-mail: weiky@ntu.edu.tw

20 Western Pacific Earth Sciences, Vol.