PAGES - Past Global Changes Magazine

PAGES - Past Global Changes Magazine

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PAGES (Past Global Changes) supports research aimed at understanding the Earth's past environment in order to make predictions for the future. We encourage international and interdisciplinary collaborations and seek to promote the involvement of scientists from developing countries in the global paleo-community discourse. PAGES scope of interest includes the physical climate system, biogeochemical cycles, ecosystem processes, biodiversity, and human dimensions, on different time scales - Pleistocene, Holocene, last millennium and the recent past. Founded in 1991, PAGES is a core project of the International Geosphere-Biosphere Programme (IGBP) and is funded by the U.S. and Swiss National Science Foundations, and the National Oceanic and Atmospheric Administration (NOAA). It is overseen by a Scientific Steering Committee (SSC) comprised of members chosen to be representative of the major techniques, disciplines and geographic regions that contribute to paleoscience.
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NEWS OF THE INTERNATIONAL PALEOSCIENCE COMMUNITYA CORE PROJECT OF THE INTERNATIONAL GEOSPHERE-BIOSPHERE PROGRAMME IGBPVol.5, N 3December 1997 PAGES International Pr oject Office, Brenplatz 2, CH-3011 Bern, Switzerland Tel: +41 31 312 3133, Fax: +41 31 312 3168, e-mail: pages@ pages, http://www. CONTENTS1PAGES activities in the Antarctic (Ian Goodwin) 2Editorial: Recent ENSO anomalies, natural variability and anthropogenic effects (R. Bradley) 5News from PEP III 6Workshop reports (LBA, LUCC/IGBP-DIS) 8Activities of PAGES lake drilling task force (S. Colman) 9PAGES calendar 10Upcoming workshops: PEP 1, agenda of the meting; Chapman Conference, conference scope 12 1st PAGES Open Science Meeting Draft program, change in the venue and general information (see also The Global Change and the Antarctic (GLOCHANT) Programme of the Scientific Committee on Antarctic Research (SCAR) co-sponsors three programmes with PAGES, on Antarctic climate and environmental history. These palaeoclimate and palaeoenvironment programmes are focused on the last 200,000 years, as recorded in deep ice cores (Palaeoenvironments from Ice Cores (PICE) programme), circum-Antarctic onshore and offshore sediments (Late Quaternary Sedimentary Record of the Antarctic Ice Margin Evolution (ANTIME) programme). A high resolution history covering the last 200-500 years and the period of greatest anthropogenic change, is the focus of the shallow to medium depth ice cores (International Trans-Antarctic Scientific Expedition (ITASE) programme). ITASE200 Years of Past Antarctic Climate and Environmental ChangeCAMBRIDGE, UK, AUGUST 2-3, 1996 As a consequence of this international meeting a science and implementation plan has recently been completed and published in the PAGES Workshop Report, Series 97-1. The ITASE Executive Summary is reproduced below. Copies of the report can be obtained from the PAGES Office, or the SCAR Global Change Programme Office, Antarctic CRC GPO Box 252-80, Hobart 7001 Tasmania, Australia.ITASE Science and Implementation Plan Executive SummaryFrom its original formulation in 1990 the International Trans Antarctic Scientific Expedition (ITASE) has had as its primary aim the collection and interpretation of a continental-wide array of environmental parameters assembled through the coordinated efforts of scientists from several nations. PAGES IN THE ANTARCTIC(continued on page 2)


2 EDITORIAL EDITORIAL Do recent ENSO anomalies reflect natural variability or anthropogenic effects or both?The strong El Nio event which developed in 1997 has wrought havoc in many parts of the world floods in Ecuador and Peru, unusually intense and frequent landfall of hurricanes in Mexico, drought and forest fires in Indonesia and Malaysia and heavy rainfall in the south-western United States. Satellite-based sensors reveal the enormous area of positive sea surface temperature anomalies which developed in the eastern Equatorial Pacific in the latter half of 1997 (see raising the question: how unusual is this situation? Satellite observations are recent and provide only a limited temporal perspective on the current event. A longer-term view is provided by the Southern Oscillation Index (SOI) which is based on the sea-level pressure difference between Tahiti and Darwin. The series extends back reliably to 1935 and although the discovery of early pressure data from Tahiti allowed a century-long series to be constructed (Ropelewski & Jones 1987) doubts have been raised about the reliability of these data (Trenberth 1997). Darwin pressure data appear to be more homogenous, but they can only provide a limited perspective on the overall complexity of the large-scale ENSO System. However, in spite of their limitations, all of these records point to the 1997-98 El Nio event as truly extraordinary comparable in magnitude to the previous record of 1982-83, but with a different temporal evolution of the anomaly field. Furthermore, the current El Nio comes on the heels of a sequence of warming events, spanning much of the period from 19901995 (Goddard & Graham, 1997); indeed, since 1976 there have been relatively few cold events and many more warm events suggesting to some that there has been a fundamental change in the climate system, brought about by anthropogenic increases in greenhouse gases. According to Trenberth & Hoar (1996, 1997) the sequence of 22 positive seasoned sea-level pressure anomalies at Darwin from 1990-95 (relative to the 1882-1981 mean) and their large magnitude, implies a return period of approximately 8850 years. They argue that such an occurrence is unlikely to be entirely due to natural variability and that anthropogenic effects are implicated. However, Rajagopalan et al. (1997) re-examine this claim using a non-parametric statistical analysis and conclude that the return period for such a sequence of anomalies is very sensitive to the statistical model applied to the data and to the reference period selected. In particular, because climate sensitivity in the Tropics consists of inter-annual, inter-decadal and lower frequency (centennial-scale) modes (Mann & Park 1994; Latif et al. 1997; Zhang et al. 1997) the calculation of ENSO return periods is a particularly difficult task when records are short. Accordingly, Rajagopalan et al. (1997) show that the 1990-95 run of positive anomalies can be viewed as having a return period ranging anywhere from 79 to 3250 years, depending on the record length and model selected.High resolution paleoclimatic data can shed light on this controversy. Geochemical studies of banded corals have demonstrated they are extremely good proxies of intra-annual changes in SST and/or rainfall in the tropics. The PAGES ARTS project (Annual Records of Tropical Systems) focuses on using such records together with tree-rings, low latitude ice cores and varved sediments to reconstruct multi-century length records of tropical climatic conditions. Research focuses on extracting reliable records of climate variability, ranging from inter-annual to century timescales. By extending the record of tropical climate variability back in time, and expanding the spatial coverage of data across the Tropics, a more comprehensive view of the spatio-temporal variability of ENSO events will be obtained. Until this happens, arguments over whether recent conditions in the Pacific are attributed to natural variability of or anthropogenic effects (or both) will be difficult to resolve.RAY BRADLEY(See page 4 for references)Chairman, PAGES SSC(continued from page 1) Because of the remoteness of the continent, Antarctica is an ideal location to monitor biogeochemical cycles and local-to-global scale climate change. However, this remoteness has also prevented the collection of instrumental records, similar to those collected in the northern hemisphere, that are required to assess Antarcticas role in and response to environmental and climate change. As a consequence ITASE has been focused to address two key scientific objectives: To determine the spatial variability of Antarctic climate (eg. accumulation, air temperature, atmospheric circulation) over the last 200 years, and where the data are available the last 1000 years. These variations include: major atmospheric phenomena such as ENSO; snow accumulation variations; and extreme events such as volcanic eruptions and storms. To determine the environmental variability in Antarctica over the last 200 yrs, and where the data are available the last 1000 years. Environmental proxies could include: sea ice variation, ocean productivity, anthropogenic impacts; and other, extra-Antarctic continental influences. In fulfilling these objectives ITASE will: produce continental scale environmental maps; elucidate transfer functions between components of the atmosphere and snow/ice; verify atmospheric models; and interpolate spatial time-series determined from satellite remote sensing. ITASE was adopted as a key science initiative by both the International Geosphere-Biosphere Program (IGBP) and the Scientific Committee on Antarctic Research (SCAR). In August 1996 a SCAR/ GLOCHANT-IGBP/PAGES sponsored workshop was held to develop this Science and Implementation Plan for ITASE. Whilst the ITASE programme will focus on obtaining a spatially contiguous Antarctic palaeoclimatic and palaeoenvironmental data set for the last 200 years, longer records spanning the last 500-1000 years will also be retrieved on an opportunity basis. The combined palaeodata set will fill a significant void in our knowledge of Antarctic climate variability. The ITASE programme is managed and coordinated through the SCAR Global Change Programme (GLOCHANT) Office, located at the Antarctic CRC in Hobart, Tasmania, Australia. All correspondence on planned and operational ITASE field traverses, firn/ice core analyses, and existing Antarctic palaeoclimatological and palaeo-environmental data banks should be made through the Programme Coordinator, Dr Ian Goodwin (e-mail: PAGES IN THE ANTARCTIC


3 PAGES IN THE ANTARCTICThis first ANTIME workshop was held in parallel with the SCAR-ANTOSTRAT (Antarctic Offshore Stratigraphy) workshop. There were 65 participants from Australia, USA, UK, Italy, Spain, Japan, Sweden, Germany and Russia. The participants included representatives of PAGES, IMAGES, INQUA and the International Arctic Science Committee (IASC). The workshop included three scientific sessions on: Extent, timing and regional differences during Glacial Stage 2 (10-30 kyr BP) in Antarctica, from the terrestrial and marine records; Climatic, environmental and glacial events during the Holocene; Late Quaternary geochronological problems in Antarctica. An abstract volume was published prior to the workshop. The participants agreed to prepare a special issue of the Antarctic Science on the most recent developments in Late Quaternary research in Antarctica. The journal issue will be edited by Ian Goodwin and Carol Pudsey from the British Antarctic Survey, and is scheduled for publication in September, 1998. An outline of the ANTIME implementation plan for fieldwork 1998-2000 was also completed and a Scientific Steering Committee was chosen from the participants. In addition, 3 sub-working groups were established on: the stratigraphic correlation of Antarctic circumpolar coastal sediments; the Late Quaternary Antarctic geochronology; glacial and sedimentological process studies. A strong linkage between the Southern Ocean component of the IMAGES deep ocean drilling programmes was developed, to extend the sedimentary record of palaeoclimate and palaeoceanography from the polar front to the Antarctic margin. A framework for an ANTIME Science and Implementation Plan was developed at the workshop. The plan is currently in development and should be published towards the end of 1998.ANTIME Priority ResearchThe workshop participants recognised that there was an immediate need to depict the present status of knowledge on the maximum extent of the Antarctic Ice Sheet during the last Glacial cycle, and the nature of the retreat to the present ice sheet margins. It was agreed that this should be completed for priority regions, which characterised the range of ice morphologies and climatologies that exist in the circum-Antarctic. These priority regions will also be used to plan future fieldwork and data correlation, and involve the linking of onshore glacial and coastal projects with marine projects on the continental shelf and slope, together with deep ocean coring projects administered through the IMAGES programme. 12 regional transects were selected as a priority for ANTIME research (Figure 1). Extensive data sets have already been collected in many of these regions, and future research is planned with national and/or international logistic support for each of these regions, over the period 1998 to 2003. The transects comprise: Region 1: Includes the Siple Coast and Siple Dome ice core record with the sedimentary record on the eastern Ross Sea continental shelf; Region 2: Consits of glacial and coastal records in Victoria Land, Transantarctic Mountains, western Ross Sea coast and continental shelf; Region 3: Covers the sedimentary record from the coastal rock nunataks, promontories and islands, and continental shelf along George V Land, Adelie Land and eastern Wilkes Land, from Cook Ice Shelf to Porpoise Bay; Region 4: Includes the Law Dome ice core record, and the sedimentary record from coastal rock nunataks, promontories and islands along the Budd Coast together with the Vincennes Bay and Totten Glacier embayments on the continental shelf; Region 5: Includes sedimentary record from the Prince Charles Mountains, Amery Ice Shelf and Embayment, Vestfold Hills lakes and fjords, Prydz Bay, and the outer continental shelf where a series of Ocean Drilling Program (ODP) drill holes are planned for the 1999-2000 season; Region 6: Links the ice core record at Dome Fuji with sedimentary record from the Lutzow-Holm Bay coast, and the continental shelf in the Cosmonaut Sea; ANTIMELate Quaternary sedimentary record of Antarctic ice margin evolutionHOBART, AUSTRALIA, JULY, 6-11, 1997(Figure 1)


4 Region 7: Links the sedimentary record in the Maudheimvidda, and offshore on the continental shelf in the Haakon VII Sea, with the potential ice core record from the planned EPICA ice cores; Region 8: Links the sedimentary record in the Shackleton Mountains with the record in the Thiel Trough, Filchner Embayment and in the eastern Weddell Sea, together with the ice core record from Berkner Island; Region 9: Covers the sedimentary record in the Ellsworth Mountains, and along the Orville and Lassiter Coasts, Region 10: Covers the sedimentary record together with the Antarctic Peninsula ice core records from two transects; the eastwest meridional record across the Antarctic Peninsula in Graham Land, and; the north south zonal record along the Antarctic Peninsula from the South Orkney Islands, South Orkney Rise, South Shetland Islands, and down the Davis and Danco Coasts. A series of ODP drill cores is planned in the Palmer Deep from which a high resolution sedimentary record is expected to cover the Late Quaternary; Region 11: Covers the sedimentary record from the eastern end of Alexander Island, with that from Marguerite Bay, and the continental shelf in the Bellingshausen Sea; Region 12: Covers the sedimentary record from the inner continental shelf in the Pine Island Glacier trough, and offshore in the Amundsen Sea. Research in these regions will include: the delineation of glacial extent and volume; the stratigraphy of glacial retreat; development of chronological control between continental shelf and onshore records; depiction of palaeo ice sheet and ice stream morphology, the relationship between ice sheets and continental shelf banks, and similarly between ice streams and shelf troughs; the interpretation of high resolution event stratigraphy for the Holocene, from: sedimentary investigations in lake, coastal, fjord, and shelf sequences; together with the high resolution ice core records from coastal ice domes. A scientific advisory committee was selected for the ANTIME programme at the Hobart workshop, such that all national programmes and Antarctic sub-regions were represented. The nominated scientific advisory committee is as follows: Prof. Eugene Domack, Hamilton College, USA, Co-Chairman, Prof. Ross Powell, Northern Illinois University, USA, Co-Chairman, Dr. Ian Goodwin, SCAR Global Change Programme/Antarctic CRC, Australia, ANTIME programme coordinator, Prof. John Anderson, Rice University, USA, West Antarctic Ice Sheet (WAIS rep), Dr. Paul Berkman, Ohio State University, USA,(continued from page 2 Ray Bradleys editorial) REFERENCESGoddard, L. & N.E. Graham 1997. El Nio in the 1990s. Journal of Geophysical Research, 102 10423 10436. Latif, M., R. Kleeman & C. Eckert 1997. Greenhouse warming, decadal variability or El Nio? An attempt to understand the anomalous 1990s.Journal of Climate, 10 2221-2239. Mann, M.E. & J. Park 1994. Global-scale modes of surface temperature variability on interannual & century timescales. Journal of Geophysical Research, 99 25819-25833. Rajagopalan, B., U. Lall & M.A. Cane 1997. Anomalous ENSO occurrences: an alternative view. Journal of Climate, 10 2351-2357. Ropelewski, C.F. & B.D. Jones 1987. An extension of the Tahiti-Darwin Southern Oscillation Index.Monthly Weather Review, 115 2161-2165. Trenberth, K.E. 1997. The definition of El Nio. Bulletin of the American Meteorological Society, 78 2771-2777. Trenberth, K.E. & T.J. Hoar 1996. The 1990-1995 El Nio-Southern Oscillation Event: Longest on Record. Geophysical Research Letters, 23 5760. Trenberth, K.E. & T.J. Hoar 1997. El Nio and climate change. Geophysical Research Letters, 24 3057-3060. Zhang, Y., J.M. Wallace & D.S. Baltisti 1997. ENSOlike interdecadal variability: 1990-93. Journal of Climate, 10 1040-1020.PAGES/GLOCHANT ACTIVITIESDr. Peter Harris, Antarctic CRC, Australia Dr. Kazuomi Hirakawa, Hokkaido University, Japan, Prof. Christian Hjort, Lund University, Sweden, Dr. Mike Bentley, University of Edinburgh, UK, Dr. Carol Pudsey, British Antarctic Survey, UK, ODP representative Antarctic Peninsula sector, Dr. Rainer Gersonde, Alfred Wegner Institute, Germany, ODP/IMAGES representative, Atlantic sector, Dr. Will Howard, Antarctic CRC, Australia, ODP/IMAGES representative, Indian and Pacific sectors, Dr. Miquel Canals, Universidad de Barcelona, Spain, and, Dr. Marco Taviani, Instituto di Geologia Marina, Italy,ANTIME Workshop Abstract VolumeLimited copies of the workshop abstract volume are available from the GLOCHANT office: Goodwin, I. D. (ed) 1997. Late Quaternary Sedimentary Record of the Antarctic Ice Margin Evolution (ANTIME), Workshop Abstracts, GLOCHANT-PAGES, Hobart, Australia, 6-11 July, 1997, 84 pp.IAN GOODWINSCAR Antartic CRC, University of Tasmania, GPO Box 252-80, Hobart, 7001, AUSTRALIA Tel: +61-3-6226 7544, Fax: +61-3-6226 7650, e-mail: RECENT PROGRESS ON ANTARCTIC DEEP ICE CORING PICEGLOCHANT/PAGES workshop on palaeoenvironments from ice coresLANZHOU, CHINA, SEPTEMBER 1998A GLOCHANT-PAGES sponsored workshop is proposed to be held in Lanzhou, China, in September 1998, in conjunction with the 6th International Symposium on Antarctic Glaciology, 5-9 September, 1998. The workshop will focus on: Comparison of regional and bipolar palaeoclimatic records over glacial cycles and the Holocene from deep ice cores; Ice-core data sharing and coordination; and, possibly Comparative ice core and marine records.For more information contact: DR DOMINIQUE RAYNAUDLaboratoire de Glaciologie et Gophysique de lEnvironnement, BP 96, 38402 Saint Martin dHres Cedex, France Fax: +33 4 76 82 42 01 e-mail: Further information can be obtained by contacting: PR. OKITSUGU WATANABEDome F Ice Core Research Group, National Institute of Polar Research, Kaga 1-910, Itabashi-ku, Tokyo 173, Japan e-mail: The Japanese Antarctic Research Expeditions (JARE) deep drilling project at Dome F (77 19 01 S, 39 42 12 E, 3,810 m) in central East Antarctica, has been completed over a 2 year period to a depth of 2,504 m. Ice core has been retrieved from the entire depth and analyses are in progress. The preliminary d18O oxygen isotope analyses indicate that the core covers the last Glacial cycle back to ~170,000 years B.P. The preliminary results were presented at the Antarctica and Global Change Symposium held at the Antarctic CRC, Hobart, Tasmania, Australia, from 13-18 July, 1997. The results confirmed that the higher snow accumulation rate at Dome F site than at Vostok, will enable a potentially higher resolution palaeoclimatic record from Dome F over the last Glacial cycle.


5 NYANZA PROJECTFive-year African lake study program funded by NSFbiological, geological and limnological research experience at Lake Tanganyika and its related lakes. Their course will consist of about three weeks of intensive laboratory and classroom training, followed by three weeks of independent research supervised by the faculty. At the same time, Cohen and program faculty will run an identical course for young African scientists with funding and research support from the United Nations Global Environmental Facility (GEF). The joint Nyanza Project fulfills part of the training mission of the International Decade of East African Lakes (IDEAL), a 5-year-old research and training consortium of African, North American and European scientists interested in all aspects of African lake science. Originally, the goal of IDEAL was to expedite a scientific program of coring the African lakes for their unique 10-million-year environmenU.S. university undergraduate students and young African researchers will study tropical lake science in a summer program based in Tanzania, on the shores of Lake Tanganyika, for the next five years. Lake Tanganyika is one of the great East African rift lakes, some of the most scientifically important and fast-changing tropical lake systems in the world. The unique program, called the Nyanza Project, will be directed by Andrew S. Cohen, Professor of Geosciences at The University of Arizona in Tucson. The National Science Foundation (NSF) recently awarded Cohen a $780,000 grant to develop an NSF Research Experience for Undergraduates (REU) program based at Tanzania Fisheries Research Institute facilities at Kigoma, Tanzania. Students will be paid for all expenses and receive stipends to work with a multinational team of instructors who have a broad range of tal record. But the consortium has expanded its focus greatly because of rapid environmental change, especially at Lake Victoria, the largest of these lakes. Scientists are trying to understand the degree to which human impact and climate are causing rapid ecosystem changes. EAST AFRICAA proposal to establish a new reference data set of climate-proxy indicators in East African lakesThe lithology of a continuous 8.20-meter long sediment profile from Crescent Island Crater in Lake Naivasha (Kenya) has produced some of the strongest evidence yet for major climatic variability in equatorial East Africa over the past 1000 years. The magnitude of reconstructed lake-level fluctuations imply that the region was much wetter than today from the mid-1600s to the mid-1700s, and that severe drought occurred during the Medieval Warm Period (about AD 1000-1250), the late 1500s, and the early 1800s. The more recent of these climatic anomalies were contemporaneous with highand lowstands of Lake Malawi and Lake Chilwa in southeast Africa that have been estimated to represent episodes when rainfall was as much as 40% higher or 70% lower than today, i.e. well beyond the long-term rainfall variability recorded in historical times. The continuity and excellent time resolution of the Crescent Island Crater record places these climatic anomalies in a chronological context that demands appreciation for the basic unpredictability of East Africas landscape resources at the scale of human generations. A collaborative effort by the University of Minnesota (USA), the University of Gent (Belgium), and Queens University (Canada) now aims to complement and further constrain the late-Holocene lake-level record of Crescent Island Crater with a reconstruction of past salinity fluctuations based on the composition of fossil diatom and chironomid assemblages. The diatom-based, quantitative paleosalinity inferences will be able to make use of known salinity optima and tolerances of diatom species derived from a reference data set of diatom floras in 164 African lakes established by Franoise Gasse and coworkers, but a comparable reference data set of chironomid faunas does not currently exist. With recent progress into the taxonomy and ecology of larval Chironomidae in African lakes increasingly revealing the potential of chironomid-based quantitative paleosalinity reconstruction in semi-arid East Africa, the author now proposes to start an extensive field survey of lakes in Kenya, Uganda, Ethiopia, and Tanzania with the purpose of collecting chironomid and water chemistry data spanning the full gradient of aquatic environments from dilute mountain tarns to hypersaline playa lakes. In consideration of the logistic effort involved (helicopters are not likely to be a regular option), it appears appropriate that a field-survey protocol be established that maximizes the usefulness of collected samples and data to the wider paleoenvironmental research community. The author therefore takes the opportunity of this announcement to invite collaboration and ideas from researchers who would like to take advantage of the proposed large-scale lake survey to collect data that may promote the interpretation (or allow calibration) of other biological and geochemical climate-proxy indicators. This research effort will take 3-4 years to complete; funding has been obtained for a first field campaign planned for the Summer or Fall of 1998.DIRK VERSCHURENDepartment of Morphology, Systematics, and Ecology University of Gent, B-9000 Gent, Belgium e-mail: PEP IIIA French version of the PANASH-PEP III report has been produced by the CST (Centre des Sciences de la Terre) in Lyon (France). Entitled Paloclimats des hmisphres Nord et Sud, le projet PANASH, les transversales Ple-Equateur-Ple (Docum. Lab. Geol. Lyon, n 146, 1997), this document is available from the PAGES office in Bern. e-mail: For further information please contact:for U.S. student inquiriesTHE NYANZA PROJECTDepartment of Geosciences University of Arizona Tucson, AZ 85721, USA Tel: (520) 626-7312 Fax: (520) 621-2671 e-mail: nyanza@geo.arizona.edufor African student inquiriesLAKE TANGANYIKA BIODIVERSITY PROJECTP.O. Box 90 Kigoma, Tanzania Tel: 255-695-2992 Fax: 255-695-2992 e-mail: or visit LTBPs Web Site at:


6 1st LBA Science Steering Committee meeting (Large scale Biosphere-Atmosphere experiment in AmazoniaSAO JOSE DOS CAMPOS, MARCH 31ST -APRIL 2ND 1997analysis. In fact, any contribution toward these objectives and the overall objectives of LBA are relevant. For example, the discussions on paleo-studies during the SSC also focused on other contributions: high resolution sonic profiles (3.5 kHz) which appear necessary for the study sites in alluvial plain; methods for providing a record of past seasonallity (speleothems, tree rings, laminated lacustrine sediment). Operations and funding are now better defined: a US contribution from NASA, mainly dedicated to atmospheric studies, but also considering ecological research (a research announcement has been made) and hydrology/ biogeochemistry. an EU contribution, to be defined during a European LBA-Worshop, in June-July. This last one, included in the G7 Pilot Project, is dedicated only to Brazil. a Brazilian consortium, to be created, including three agencies (FINEP, FAPESP, CNPQ) other contributions are from IAI and some European projects. From an operational point of view, the European funding is, for the moment, restricted to Brazilian sites. For paleo-studies it may offer opportunities for European research in cooperation with Brazilian Institution, but many important EU contributions in other Amazonian countries have to be included in further projects. At the moment, specific research projects linked to the German Program SHIFT or to the French Program, from ORSTOM, AIMPACT, are capable of contributing to integration of the European LBA. Many objectives of LBA paleo-studies cannot be restricted to Brazil or US or EU operations. One of the most important is the creation of a data bank of present-day pollen deposition, which is also an objective of the PAGES and GCTE Core Projects of IGBP. Such an objective requires full participation by all Amazonian palynologists, in conjunction with Botanists, Climatologists and Statisticians. An effort must then be made, by the scientific community, for the integration of research funded by different countries (Brazil, USA, EU). The sites for paleo-environment and paleo-climate studies should be, if possible, close to the LBA study sites (where all other researches are centered). The sites chosen during this SSC meeting were Rondonia Sao Gabriel da Cachoeira, Tefe (Mamiraua), Manaus, Santarem, Maraba and Brasilia, this last one representing the extraAmazonia reference site. For neighbouring countries, some sites have been cited: Noel Kempf Reserve (NE Bolivia), Sao Carlos do Rio Negro (Venezuela), Puerto Maldonado (Peru), Napo Valley (Equador), Leticia and Araracuara (Colombia). In the physical climate realm, comparisons may be made on a larger space scale, Amazonia climate variations should be compared with extra-tropical records. My final consideration would be that a clear call has been made by the LBA, to the paleo-community. This is an excellent opportunity to demonstrate the utility of paleoenvironmental reconstructions for a better understanding of the current and future behavior of environmental systems. This regional approach provides a favourable opportunity to put different fields of science in contact with each other.BRUNO TURCQORSTOM-UFF Departamento de Geoquimica Morro do Valonguinho s/n, 24020-007 Niteroi, Brazil e-mail: The key questions for LBA are: How does Amazonia currently function as a regional entity? How will changes in land use and climate affect the biological, chemical and physical functions of Amazonia, including the sustainability of development in the region and the influence of Amazonia on global climate? The LBA is divided in six general areas:Physical Climate (which currently included the paleoclimate studies); Carbon Storage and Exchange; Biogeochemistry; Atmospheric Chemistry; Land Surface Hydrology and Water Chemistry; Land Use and Land Cover The LBA has been endorsed by IGBP as the first Integrated Global Change Science Project. Paleoclimate and paleo-environment studies are definitively included in the LBA frame, linked questions are described in the LBA Integrated Science Plan, soon to be published: 1. What have been the patterns of climate change (precipitation and temperature) on millennial to century time-scales in the Amazon environment? 2. How will analogues of past conditions, which generally represent an average of climate during several decades, help to improve our understanding of large scale mechanisms? (e.g. similarities have been observed between some climate variations during the last 7,000 years and present-day El Nino events). 3. What is the relative importance of external forcing (e.g. changes in insolation, atmospheric CO2, SST) vs internal mechanisms for Amazon paleo-situations? 4. What have been the impacts of extreme climate variations during the last millenia on Amazon environments (vegetation changes, fires, erosion). A previous document (LBA scientific meeting) gave emphasis to lacustrine studies and sedimentological/palynological proxies. The new text also includes other methodologies such as: physical geography, fluvial geomorphology, biogeography of vertebrates, soils and soil organic content (13C, 14C, charcoal). Other South American records, including volcanic activity and Andean ice cap cores, must also be considered in ourSpatial-Temporal Dimensions of High-Latitude Ecosystem ChangesKRASNOYARSK, RUSSIA, SEPTEMBER 2-7, 1997The Institute of Forestry, Krasnoyarsk, recently hosted a workshop on SpatialTemporal Dimensions of High-Latitude Ecosystem Changes as a contribution to the development of the IGBP North Siberian Transect. PAGES was represented by expertise in dendro-climatology (notably Keith Briffa, University of East Anglia and Malcolm Hughes, University of Arizona, in addition to members of the Forestry Institute under Eugene Vaganovs leadership) and in peat and sediment studies. The programme included an excursion to contrasted forest sites in the region and a wide range of scientific presentations and discussions. Recognition of the vital role of dendro-research in establishing fire histories, the nature of disturbance regimes and forest stand dynamics at the patch scale, as well as in providing high resolution paleoclimatic information and estimates of changingWORKSHOP REPORTS (continued top of next page)


7 The importance of studying long term records of land-use/land-cover (LU-LC) change was acknowledged at the meeting. One goal shared by LUCC and PAGES will be to document, by all available means, the history of LU-LC change over the last 200 years. This is in accordance with the views expressed more widely at the IGBP Congress in 1996. The spatial cover will ideally be global, though regional disparities in data are recognised as a significant limitation for some parts of the world. In order to achieve this initial goal, it will be necessary to generate a common commitment between interested groups in LUCC and PAGES, which, in turn, implies developing the initiative in ways that can generate mutual benefits to both communities. As a first step, it was proposed to hold a small workshop (10-12 people) with, as its proposed title: Historical Dynamics of Land Use, AD 1800 to 1997 The main aims of this would be to: define and start to establish a collaborative community willing and able to carry the initiative forward; address, as required, the question of data calibration with respect to fully documented LU-LC categories at the present day and in the recent past; define and promote rationales for the initiative that would attract broad support and participation; create classification schemes directly linked to LUCC activities and priorities; resolve issues of spatial scale and temporal resolution; establish guidelines for regional and methodological contributions and for harmonising these to create a global data set; identify and build on existing data sets. The likely participants in such an initiative are quite diverse, as are the types of data they use and the insights they can provide. They include, for example, pollen analysts, historical geographers, environmental historians, dendro-ecologists and landscape ecologists. Harmonising the interests, skills and data output of such a disparate group is a non-trivial task. The most practical product of the initiative would be a spatially referenced data base from which a series of time-slice maps, for example,Land Use and Land Cover Change (LUCC) / IGBP-DIS Data Requirements WorkshopBARCELONA, SPAIN, NOVEMBER 11-14, 1997 PAGES presentations were made by Suzanne Leroy and Frank Oldfieldcould be generated at any stage and refined as the project progressed. It was suggested that DIS, LUCC, PAGES, GAIM and GCTE were all potential participants from within IGBP. Any members of the PAGES community who are interested in taking part in such an initiative should contact the Project Office. Other PAGES-related themes that were considered included: the need for longer term perspectives, especially in ecosystems like forests, where successional/competitive processes took place over longer periods of time. In such cases, biophysical feedbacks, species composition and ecosystem structure and function may change on relatively long time scales and a perspective from 200 to 1000 years was considered desirable; the importance of studies documenting nonreversible human impact on fragile ecosystems in the past; the need to include a well articulated historical dimension in regional case studies of special significance to LUCC; the value of exploring the impact of natural climate variability on LU-LC.FRANK OLDFIELDExecutive Director PAGES IPO e-mail: PAGES International Project Office Brenplatz 2 CH-3011 Bern, Switzerland Tel: +41 31 312 3133 Fax: +41 31 312 3168 e-mail: Executive Officer: Frank Oldfield Director: Bruno Messerli Scientific Assistant: Keith Alverson Office Manager: Niklaus Schranz Publication Officer: Cindy Jones Newsletter Editor: Frank OldfieldPrinted on recycled paper WORKSHOP REPORTSbiomass, was one of the clear highlights of the meeting. Carbon sequestration in boreal ecosystems was a major linking theme of the workshop and the complementary roles of forest, soil and peat studies were emphasized. The potential role of peat, hydromorphic soil and lake sediment studies in reconstructing not only past vegetation and forest dynamics but also mineral flux, within defined watershed-ecosystems, was accepted as a component of the implementation plan for the transect. The environmental context provided by the North Siberian transect is rich in paleoarchives and is one where there is every opportunity for PAGES science to interact with other parts of IGBP, notably GCTE and BAHC. The meeting also gave an opportunity for the assembled scientists to celebrate the honour recently achieved by one of the retiring PAGES Scientific Steering Committee members, and Director of the Institute of Forestry, Dr. Eugene Vaganov, namely his election as an Academician.FRANK OLDFIELDExecutive Director PAGES IPO e-mail: C-T. A. Chen and T. Hama awarded Biwako PrizeThe Biwako Prize for Ecology was founded by the Shiga Prefectural Government of Japan in 1991 in the hope of contributing to the progress of aquatic environment studies in the fields of limnology, oceanography, ecology and related sciences. Biwako means Lake Biwa, the largest lake in Japan and the third oldest in the world. Each year a certificate of merit and five million Japanese yen (about $ 40,000 US) are awarded to two researchers chosen by the Shiga Prefectural Government and the International Lake Environment Committee. This year recipients were Dr. ChenTung Arthur Chen of the Institute of Marine Geology and Chemistry, National Sun Yat-sen University, Taiwan and Dr. Takeo Hama of Nagoya University, Japan. Dr Chen was noted for his research related to the oceanic CO2 problem and PAGES related work in the lacustrine environment in Taiwan. Dr. Hama was noted for his research on primary productivity in the oceans.


8 Origin of the Lake Drilling Task ForceBecause successful acquisition of long continental paleoclimate records requires major investments in planning, logistics, and drilling technology, it is important to select the most promising sites, to conduct pre-drilling site evaluations, and to select the most suitable drilling technology. To facilitate a coordinated selection process, participants at the PAGES Workshop on Continental Drilling for Paleoclimate Records (see PAGES Workshop Report Series 96-4, WWW address below) agreed to form a Task Force to organize a coordinated Global Change initiative for national and international funding agencies. A particular target for engagement was the then-emerging International Continental Scientific Drilling Program (ICDP). The goal of the Lake Drilling Task Force is to provide some coordination for the notoriously fragmented continental paleoclimate community, and to facilitate large-scale international efforts to retrieve long (ca. 250 kyr) lacustrine records analogous to those generated by the marine and ice-core communities. The Task Force promotes the development of a regional network of long, continental paleoclimate records, closely associated with the Time Stream II activities and priorities of the PEP transects. With respect to ICDP, we hope to form partnerships between ICDP, which would support drilling operations and technology, and national or international science funding agencies, which would provide support for scientists and analytical work. Individuals serving on the Task Force are the leaders of PEP I (V. Markgraf), PEP II (J. Dodson and Liu Tungsheng), and PEP III (F. Gasse), along with several people associated with large lake coring or drilling projects and related activities (D. Williams, T. Johnson, J. Negendank, S. Leroy, and S. Colman). Doug Williams served as head of the Task Force through November, 1996; Steve Colman now serves in this capacity.ICDPThe International Continental Scientific Drilling Program (ICDP) grew out of the need for a continental version of the Ocean Drilling Program. Its origins lie largely in the deep crustal drilling community, especially the U.S. Continental Scientific Drilling Program and the German KTB Drilling Program. ICDP was formally launched by a memorandum of understanding between the U.S. and Germany in 1996. It operates on funds contributed by membership fees, on a sliding scale, decreasing from the current fee of 700,000 US$ for G7 countries. Initial members were the U.S., Germany, and China. Countries likely in the near future include Japan, Mexico, Russia, a consortium of small European countries, and UNESCO (for developing countries). The organization is run by an Executive Committee consisting of one representative from each member country. Proposals are reviewed by a Science Advisory Group, which makes funding recommendations to the Executive Committee.HistoryUnder the leadership of Doug Williams, the Task Force solicited from the continental paleoclimate community two-page proposals for lakes that should be considered and prioritized for drilling support by ICDP. The proposals included a brief description of the lake(s) of choice; the rationale for selection in terms of scientific questions to be addressed, prospects for success, and logistical challenges anticipated; a list of participating scientists, and an estimated budget. More than 60 of these mini-proposals were submitted to the Task Force and were reviewed at a meeting of the Task Force in October, 1995. The Task Force evaluated the proposals primarily on the basis of the likely quality of the paleoclimate records to be obtained, the scientific importance of records from particular sites, and the relation of particular sites to the goals of the PEP transects. To some degree, the readiness of proposed projects affected the order of priority among the highest rated proposals. More complete proposals were requested for lake sites evaluated as having the highest priority by the Task Force. These materials were compiled into a five-year drilling plan, which was presented to ICDP at the VIII International Continental Drilling Symposium in February, 1996, in Tsukuba, Japan. The plan was also circulated to the international community for additional input. In response to ICDPs initial call for pre-proposals, the plan was submitted to ICDP in April, 1996, as a Prospectus for a Global Lake Drilling Initiative. At the same time, individual proposals were submitted by the leaders of six lake drilling projects, five of which were among those evaluated by the Task Force and included in the Prospectus. The Task Force Prospectus proved difficult for ICDP to handle, so ICDP did not consider the Prospectus nor the included projects in its review of original pre-proposals. In order to resolve this problem and other concerns related to PAGES projects, including length of record and the inclusion of tectonic studies, ICDP funded a workshop, which was held at Lamont-Doherty Earth Observatory in December, 1996, attended by all of the PAGES Task Force members. Information concerning this Workshop, including a draft report, is available on the World Wide Web (address below). The meeting resulted in a clearer understanding of the priorities of ICDP and a greater appreciation for the importance of lacustrine paleoclimate records. One of recommendations of the Lamont workshop was that a PAGES representative be appointed to the Science Advisory Group of ICDP, the group that reviews proposals. Steve Colman was asked to fill this role and joined the SAG for its yearly review of proposals (submission deadline 15 January). Remarkably, eight proposals related to paleoclimate records from lakes were submitted to ICDP, representing almost half of all drilling proposals. Out of the proposal process, the Baikal Drilling Project received substantial funding for core-logging equipment, the Lake Titicaca and IDEAL projects received limited funding for workshops and (or) engineering studies, and a planning workshop was recommended for the Qinghai Lake (China) project. Some problems, such as participation in ICDP by small developed countries (e.g. New Zealand) remain, but are being addressed.Recent developmentsIn response to the many high-quality lakedrilling proposals, particularly the favorable reviews of the East African lakes (IDEAL) and Lake Titicaca proposals, ICDP is proceeding with development of technical and engineering capabilities for drilling medium to large lakes. They supported a small workshop in Miami in October, 1997, organized by Chris Scholz, which included engineers from ODP and industry (WWW information below). This faceto-face discussion between scientists and engineers was extremely productive and resulted in a recommendation for a formal feasibility study of the costs and performance of different systems for drilling the lakes in question. ICDP agreed to fund the study, and the request for proposals has been issued. The award is expected to be made in December, 1997 and the results are expected in March, 1998. We are now confident that one of these lakes, probably Lake Edward, will be drilled in the near future, possibly as early as 1999. The next round of proposals for ICDP is due January 15, 1998. In the meantime, the Lakes Drilling Task Force will continue to seek ways to promote the drilling of lakes for paleoclimate records in general, as well as providing an interface to ICDP. CONTINENTAL DRILLING FOR PALEOCLIMATE RECORDSActivities of PAGES Lake Drilling Task ForceCONTINENTAL DRILLING(continued on page 9 col. 1, bottom)


9 Additional information (WWW) ICDP and proposals: Lamont ICDP Workshop: nbcp/lake.html (including draft report) Miami ICDP Workshop: PAGES Task Force: pages/ldtf.html (includes links to other related items) PAGES Workshop Report 96-4: Workshops/Contidrill/0toc.html INSIDE PAGESChanges at the PAGES IPO1997 has been a year of considerable change at the PAGES IPO. Ulrich Schotterer has concluded his role as PAGES scientific assistant. As well as continuing to work towards the enhancement of the Global Network for Isotopes in Precipitation, he will also concentrate his efforts on a new, independent, scientific initiative on Isotopes in the Hydrological Cycle (ISOHYC). In his place, PAGES welcomes Keith Alverson a physical oceanographer with interests in oceanic convection, air-sea interaction, and the application of inverse modelling techniques to paleoclimate model-data comparison problems. Finally, PAGES has benefited enormously from the hiring of Niklaus Schranz as office manager. Niklaus has a background in geography and brings strong electronic communications skills to the office. PAGES CALENDAR(*: Open meetings. All interested scientists are invited to attend) *February 9-2, 1998 Boulder, CO, USA Second Workshop on Global Paleoenvironmental Data Contact: Robin Webb or Dave Anderson. Tel: +1 303 497 6160; Fax: +1 303 497 6513; e-mail:, *February 16-20, 1998 Chiang Mai, Thailand Southeast Asian Dendrochronology Workshop (SEA Dendro 98) Contact: Rosanne DArrigo, Tree-ring lab., Lamont-Doherty Earth Observatory, Palisades, USA. Tel: + 914 365 8617; Fax: + 914 365 8152; *March 14-18, 1998 Barcelona, Spain GCTE-LUCC Science Conference (Global Change in Terrestrial Ecosystems-Land Use/Cover Change) Contact:Will Steffen, GCTE Core Project Office, CSIRO Division of Wildlife & Ecology, PO Box 84, Lyneham, ACT 2602, Australia. Fax: +61 1 241 2362, e-mail:; conference98.html *March 16-20, 1998 Merida, Venezuela PEP 1 Meeting Contact: Dr. Vera Markgraf, INSTAAR, University of Colorado, Boulder CO 80309 0450, USA. e-mail; *April 19-23, 1998 London, UK First PAGES Open Science Meeting ***New Location*** Senate House, University of London, UK Contact: Frank Oldfield, PAGES IPO, Switzerland. Tel: +41 31 312 3133; Fax: +41 31 312 3168; e-mail:; *May 18-21, 1998 Yarmouk University, Irbid, Jordan Learning from the Past: Global Paleoclimatic Changes Contact: Prof. Ali Jawad Ali, Faculty of Science,Yarmouk University, IRBID, Jordan. Tel: +962 2 271100; Fax: +962 2 247983/274725; e-mail: May 16-23, 1998 Torshavn, Faroe Islands Environmental Change in Atlantic Islands Contact: C. Caseldine, University of Exeter, UK. Tel: +44 1392 263 347; Fax: +44 1392 263 342; e-mail: *June 14-18, 1998 Snowbird, Utah, USA Chapman Conference on Mechanisms of Millennial-Scale Global Climate Change Contact: AGU Meetings Department, Millennial-Scale Global Climate Conference, 2000 Florida Av, N.W., Washington, D.C. 20009, USA. Tel: +1 202 462 6900; Fax: +1 202 328 0566; e-mail: July 2-7, 1998 Perth, Australia PEP-II Workshop in Variability of Southern Hemisphere Climate Systems and Linkages with Northern Hemisphere Systems, on Time Scales covering the last two Glacial Cycles University of Notre Dame, Fremantle Contact: John Dodson. e-mail: *July 6-10, 1998 Exeter, UK Hydrology in a Changing Environment Contact: Dr Bruce Webb, Department of Geography, University of Exeter, Armory Building, Rennes Drive, Exeter, Devon, EX4 4RJ, UK. Fax: +44 1392 263342; e-mail:; *July 27-August 7, 1998 Lanzhou, P.R. China, International Symposium and Field Workshop on Paleosols and Climatic Change Contact: Pr Fang Xiaomin, Lanzhou Univeristy, Lanzhou, Gansu Province 730000, P.R. China. e-mail: *August 23-28, 1998 Lisbon, Portugal International Conference on Paleoceanography ICP VI Contact: F. Abrantes. e-mail: *September 5-7, 1998 Puerto Vallarta, Mexico 15th AMQUA Biennal Meeting on Northern Hemispheric-Southern Hemispheric Interconnections Contact: Dra. Socorro Lozano Garcia. e-mail:; Fax: +52 5 550 6644; September 7-11, 1998 University of East Anglia, Norwich, UK Climate and History: Past and Present Variability A Context for the Future Contact: Susan Boland, Climatic Research Unit, University of East Anglia, Norwich, NRA 7TJ. Tel: +44 1603 456161; Fax: +44 1603 507784; e-mail:; *August 3-11, 1999 Durban, South Africa The Environmental Background to Hominid Evolution in Africa INQUA XV International Congress, International Congress Centre Durban Contact: Dr D.M. Avery, Secretariat General, South African Museum, P.O. Box 61, Cape Town 8000, South Africa. Tel: +27 21 243330; Fax: +27 21 24671; e-mail:; Center for Field Research invites proposals for 1998-99 field grants funded by its affiliate Earthwatch. Earthwatch is an international, non-profit organization dedicated to sponsoring field research and promoting public education in the sciences and humanities. Past projects have been successfully fielded in, but are not limited to the following disciplines: aquaculture, limnology, marine resource conservation, oceanography (chemical, biological and physical) and marine geology. Interdisciplinary projects are especially encouraged as is multi-national collaboration.Information can be found at: THE CENTER FOR FIELD RESEARCH, 680 Mt. Auburn St., Watertown, MA 02272, USA; Tel: (617) 926-8200; Fax:(617) 926-8532; Center for Field Research invites proposals for 1998-1999 (continued from page 8)


10 PEP 1 Paleoclimates of the AmericasMERIDA, VENEZUELA, MARCH 16-20, 1998UPCOMING WORKSHOPSTo further our understanding of interhemispheric climate linkages in the Americas, present and past, a meeting is convened in Merida, Venezuela, March 16 to 20, 1998. The meeting represents the first attempt to address the goals defined by the IGBP-PAGES initiative Pole-Equator-Pole Paleoclimates of the Americas (PEP 1).MODERN CLIMATE VARIABILITYHenry Diaz, coordinator Miguel Acevedo, Rigoberto Andressen, Kent MCGregor, Hirma Ramirez and Magdiel Ablan: Climate Variability Scenarios for the Llanos of Venezuela: Soil Moisture and SST anomalies Mike Dettinger and Dan Cayan: Historical Modes of Interannual and Decadal Hydroclimatic-Hydrologic variability in the Western Hemisphere Dave Enfield: Western Hemisphere Modes of Ocean-Atmospheric Co-Variability Stefan Hastenrath: Atmospheric Circulation of the Tropical Americas Jose Marengo: Cold Front and Polar Advections in the Americas during Modern and Past ClimatesLAST 2000 YEARS CLIMATE VARIABILITYMalcolm Hughes, Tim Baumgartner and Lonnie Thompson, coordinators Jose Boninsegna and Malcolm Hughes: Tree Ring Records from the Americas Tim Baumgartner and Marco Salamanca: Developing a Paleoclimate Transect for Marine Sites along the Eastern Pacific Margin Tim Baumgartner, Andy Soutar and F. Ferreira: Patterns of Interhemispheric Climate Change of the Past 2000 Years Inferred from high-Resolution Marine Sediment Records of the Eastern Pacific Thomas Kitzberger, Thomas Swetnam and Thomas Veblen:A Comparison of Fire Histories and Climatic Change in the Southwestern United States, and Northern Patagonia, Argentina Brian Luckman: Assessing Synchroneity of Glacier Fluctuations in the Western Cordillera of the Americas during the Last Millennium Lonnie Thompson: Climate of the Last 2000 Years in the Tropical Andes of South America Sheri Fritz: Moisture Patterns in the Americas over the Last 2 Millennia Inferred from Lacustrine RecordsENSO CLIMATE VARIABILITYRobert Dunbar, coordinator Dave Battisti: Climate Phenomenon on Interannual to Decadal time scales that have Interhemispheric Impacts on the Americas Julie Cole and Ed Cook: Changing Relationship between ENSO and North American Drought Alexey Kapan: Globality and optimality in climate fields reconstructions: ENSO and more Luc Ortlieb: Historical Records of ENSO Ricardo Villalba, Rosanne DArrigo, Ed R. Cook, G. Wiles and G. Jacoby: Decadal-scale Climatic Variability along the Extra-tropical Western Coast of the Americas over Past Centuries inferred from Tree-ring Records Rosanne DArrigo and D.W. Stahle: Multiproxy Reconstructions of the Southern OscillationHUMAN DIMENSIONSDiana Liverman, coordinator Diana Liverman: The Human Dimensions of Global Change in the Americas: An Overview Mark Brenner, Hodell, D.A., Leyden, B., Curtis, J.H., Binford, M.W., Kolata, A.L. and Abbott, M.B.: Environmental Determinism Revisited: Climatic Limits on Cultural Development Lautaro Nunez: Eventos de Aridez Pleistoceno-Holocenicos en el Centro-Norte de Chile y su Correlacion con los Primeros Poblamientos del Cono Sur Roberto Sanchez: Vulnerability of Latin American Cities to Climate Change and Climate Variability Payson Sheets: The Effects of Explosive Volcanic Eruptions on Simple-toComplex Societies in Ancient Middle AmericaMID-HOLOCENE CLIMATE VARIABILITYJulio Betancourt, Wolfgang Volkheimer, coordinators Walter Dean, Sarah Metcalf, Philippe Mourguiart: Lacustrine Records of Mid-Holocene Climates of North America Eric Grimm and Socorro Lozano-Garcia: Vegetational Signal in the Americas of Geographically Variable Climate Forcings during the Mid Holocene Dan Muhs: Late Quaternary Eolian Records in North America with a Comparison to Eolian Records in South America; Marcelo Zarate: Late Pleistocene and Holocene Eolian Records of Southern South America (The Pampas and the Chaco Region) Jan Heine: Mid-Holocene Glacier Advances in North America; Geoff Seltzer:Holocene Glaciation in Central and South AmericaLATE GLACIAL CLIMATE VARIABILITYHenry Hooghiemstra, Vera Markgraf, Cathy Whitlock, coordinators Platt Bradbury: Late-Glacial (15 8 ka) Lake Records along PEP 1 Transect: Their Role in Developing Inter-hemispheric Paleoclimate Interactions; Martin Grosjean: Late Glacial and Holocene Climate Changes on the Southern Altiplano (20-28S) Marie Pierre Ledru and Maria Lea Salgado-Labouriau: Vegetation Records in North and South America Scott Lehman and Carlos Herguera: Marine Records Dorothy Peteet: Late-Glacial Climate Variability GCM Modeling Experiments Geoff Seltzer: Late Glacial Glaciaton in Central and South America; Jan Heine: Late-Glacial Glaicer advances in North America Jim White: Polar Ice Core Records J.M. Pajon and F. Ortega: Paleoclimatic and Paleoenvironmental Studies in CubaFULLGLACIAL CLIMATESThomas Pedersen, Miguel Angel Gonzalez, coordinators Allan Ashworth: A Comparison of the Beetle Faunas of the Last Glaciation from the Mid-latitudes of North and South America Chalmers Clapperton and Max Bezada: Full-Glacial Glacier Extent and Chronology along the PEP 1 (Americas) Transect Jim Kennett: Late Quaternary Climate and Ecosystem Instability: Southern California Margin M.A. Gonzalez: Lake Records of the Americas Todd Sowers: Interhemispheric Linkages during the Last Glacial period Robin Webb: High versus Low Latitude Glacial Climate Sensitivity in the Americas: Results from PMIP Simulations and Other Sensitivity Experiments Cathy Whitlock: Features of the Full-Glacial Vegetation of the Americas Michel Servant: Comparison of Fullglacial Climatic Features in South America and AfricaPEP 1 Meeting Agenda These goals are: 1) to document the inter-relation between climate change patterns in the Americas in terms of amplitude, phase, and geographic extent; and 2) to determine the forcing factors which affected each hemispheres as well as the interhemispheric climate change patterns. Sixty-two speakers have accepted the invitation to present an inter-hemispheric overview of climate change and climate variability from instrumental climate, terrestrial, ice core and marine records in the Americas, for specific time intervals, present and past. In addition, 28 posters have been submitted for the poster session, representing specific the sessions topics. From the meeting a book will be produced, containing chapters on the sessions topics.


11 UPCOMING WORKSHOPSConference Scope:This conference will provide an international forum for discussion of possible mechanisms that may account for millennialscale climate change. Unlike orbital-scale climate change, which has a well-defined forcing mechanism in changes in solar insolation, the cause(s) of millennial-scale climate variation remain(s) unknown. The growing global paleoclimate database relevant to this issue is now of significant breadth to provide the critical information required to address these issues. The central themes of this conference will address two key questions that arise from evidence of millennial-scale climate change: (1) What is the sensitivity of various components of the Earths climate system to millennial-scale climate change? (2) What are the mechanisms, linkages, and feedbacks which produce millennial-scale climate change? A subset of these general themes includes: Is millennial-scale climate change a characteristic only of ice-age boundary conditions, or do those conditions simply amplify an ongoing process? Is millennial-scale climate change globally synchronous? If so, is the change symmetrical (of equal sign) across both polar hemispheres? Are the linkages made through theChapman Conference on Mechanisms of Millennial-Scale Global Climate ChangeSNOWBIRD, UTAH, USA, JUNE 14-18, 1998 Cliff Lodge Snowbird Conference Center CONVENERS: Peter U. Clark, Department of Geosciences, Oregon State University, Corvallis, OR, USA Robert S. Webb, NOAA-NGDC Paleoclimatology Program, Boulder, CO, USA PROGRAM COMMITTEE: Richard B. Alley, Antony J. Broccoli, Wallace S. Broecker, William Curry, Laurent Labeyrie and Alan Mix EUROPEAN ACTIVITIES NETHERLANDS FOUNDATION FOR SCIENTIFIC RESEARCH (NWO) FUNDS IMPLEMENTATION OF PAGES RESEARCHClimatic change at low elevation: expedition to the savannas and rain forest of ColombiaPaleoecological and paleoclimatological knowledge of northern South America is mainly based on Andean studies. Current key questions concern especially the lowlands. It is still not clear how much tropical lowlands cooled during the last glacial maximum (LGM) and to what degree changes in precipitation were relevant. The changes were possibly more than first CLIMAP estimates of <2 C, perhaps less than 8 C often claimed in palynological studies from the Colombian Andes. Recently, a cooling of Amazonan lowlands by 4 C for the LGM is claimed by both schools debating the Amazonian refuge theory. Also for paleodata-model comparisons reliable paleo-vegetation maps are missing. The Netherlands Foundation for Scientific Research (NWO), Geological, Oceanographic and Atmospherical Research branch (GOA), funded the post-doc project Paleo-ecology of 0-20 kyr tropical America based on new pollen records and integration of existing palynological data for 3 years. A field expedition to the savannas of the Llanos Orientalis, and the rain forest of Choco was part of the project. We aimed to core the maximum number of lakes and swamps in order to give expensive expeditions the maximum scientific effect. During January-February 1996 we visited with two 4-wheel-drive cars and our new Livingstone Corer (modified by Paul Colinvaux) the savannas of NE Colombia, mainly at 150-200 m altitude. Over a transect of 600 km we cored 12 lakes. Core length varied from 10 m close to the Eastern Cordillera to 1 m in the centre of the Llanos. First radiocarbon dates show most cores represent the last 8,000 to 12,000 years, one core reaches 18,000 years showing the savanna in the LGM. In August 1996 we visited the interAndean valleys of the Rio Cauca and Rio Patia in southern Colombia. We cored 4 peat bogs at 1020 m altitude in the humid Cauca Valley. Cores were 2 to 7 m long and first radiocarbon dates show these records reach 8,000 to 13,000 years back in time. In the dry Patia Valley we cored 4 lakes at 760 m altitude. Cores were 3 to 5 m long and first radiocarbon dates show these records reach 6000 to 11,000 years back in time. During January-February 1997 we had our most difficult expedition to the Pacific rain forest of Choco. Travel, organisation and physical conditions were challenging. We cored a lake in each of the 3 provinces that constitute the Choco biogeographic area. The 3 cores are 5 to 6 m in length. One core was raised with the Livingstone Corer from 23.5 m water depth. Perhaps these cores will help us to discover why the Choco rain forests have the largest biodiversity in the world. Expertise at the Hugo de VriesLaboratory concerns pollen analysis and time control. But we would be delighted if other colleagues are interested to make use of our core material to study additional proxies, such as diatoms, phytoliths, geochemistry, etc. Especially colleagues in the PEP-1 community are invited to contact us to discuss proposals for joint studies. atmosphere, the deep and surface ocean, or both? If globally synchronous, does millennialscale climate change represent an internal climate oscillator originating in the North Atlantic region and transmitted globally through the atmosphere and oceans? Does millennial-scale climate change represent a common global forcing mechanism transmitted from the tropics? Do changes in the southern hemisphere drive climate change elsewhere? What are the feedbacks between various components of the Earths climate system at these timescales? Does all millennial-scale climate change share a common forcing (internal or external), or do several possible forcing mechanisms exist which independently produce millennial-scale climate change?For further information please contact: AGU MEETINGS DEPARTMENTMillennial-Scale Global Climate Conference 2000 Florida Avenue, NW Washington, DC 20009, USA Tel: (202) 462-6900 Fax: (202) 328-0566 e-mail: PROF. DR. HENRY HOOGHIEMSTRAHugo de Vries-Laboratory The Netherlands Centre for Geo-ecological Research (ICG) University of Amsterdam Kruislaan 318 1098 SM Amsterdam, The Netherlands Tel: 31 20 525 7857 Fax 31 20 525 7662 e-mail:


12Putting PAGES togetherFor the first time since the establishment of its program of Foci and Activities, PAGES has held a meeting of virtually all the scientists responsible for coordinating PAGES research throughout the world. This Leaders Meeting took place in Hilterfingen, Switzerland on the north shore of Lake Thun, November 8 and 9, 1997. The main goals of the meeting were to summarize progress in each area of activity, to review the PAGES project as a whole, to promote synergism between the various research teams and to put PAGES on course for making the best possible impact at the Open Science Meeting. PAGES derives its distinctive identity from prioritizing the study of those aspects of past global change that contribute crucially to our understanding of Earth system function on human timescales and to our capacity to improve the quality of any assessment of future climate changes and their impacts. Even with this strongly focused research agenda, the range of tasks to which PAGES is committed is broad and diverse. The challenge of synthesizing the results is a daunting one. Full documentation of all the PAGES activities will soon be available through publication of the PAGES Status Report and Implementation Plan now complete and due for publication early in 1998. To some degree, the structure of PAGES includes built-in patterns of coordination. Some of these, like PEP I are already at the stage where preliminary syntheses can be attempted (see Calendar entry on the Merida Meeting ). Beyond these, the PAGES Open Science Meeting to be held in London April 20 23, 1998, will provide an over-arching compilation of PAGES science and of its significance for the future (see this page). In parallel with presentational syntheses at meetings and in the publications that grow out of them, PAGES shares an additional key responsibility: the WDC-A Paleoclimate Data Base which can be accessed via either NGDC in Boulder Colorado (http://www.ngdc.noaa .gov/paleo/igbp-dis/index.html) or MeteoFrance in Toulouse, France (http://www. constitutes a major global resource and a long term PAGES legacy of growing value. Efforts are underway to ensure that the facility meets the data needs of all PAGES research. The Data Workshop in Boulder, (February 9 12, 1998) is an important stepping stone in this direction. PAGES OPEN SCIENCE MEETINGSenate House, University of London, April 20 23, 1998 DRAFT PROGRAMMONDAY APRIL 20 8.45 9.25Ray BradleyIntroductory overview 9.25 10.05Keith BriffaAnnual climate variability in the Holocene; interpreting the message of ancient trees. 10.15 10.45Mike GaganCorals: grand archives of tropical paleoclimateCoffee break11.15 11.55Lonnie ThompsonIce core evidence for climate change in the Tropics: Implications for our future 11.55 12.35Vera MarkgrafInterhemispheric paleoclimate linkages and forcing in the Americas from decadal to millennial scalesLunch14.00 14.40Zhisheng AnThe history and variability of East Asian monsoon climate 14.40 15.20Franoise GasseThe temporal evolution of African climates based on lake system records 15.20 16.00Jim KnoxMagnitudes and spatial patterns of Holocene hydrologic sensitivities to global climate changes 16.00 18.00 Poster session 1 TUESDAY APRIL 21 8.45 9.25Richard AlleyAbrupt climate changes of the past and the future? lessons from the Greenland ice cores. 9.25 10.05Elsa CortijoRapid climatic variability of the Atlantic Ocean and global climate: a focus on the IMAGES program. 10.05 10.45Dominique RaynaudThe past record of greenhouse gases: a view in the context of future changesCoffee break11.15 11.55Juerg BeerThe role of the sun in climate forcing 11.55 12.35Greg ZielinskiDetermining the range of variability in the volcanism-climate system through multi-disciplinary evaluations of explosive eruptions over the last 100,000 yearsLunch14.00 14.40Thomas StockerPast and future reorganizations in the climate system. 14.40 15.20Suki ManabeThe study of abrupt climate change by a coupled ocean atmosphere model 15.20 16.00Edouard BardComparing temperatures of the glacial ocean quantified with the alkenone method and simulated by numerical models 16.00 18.00 Poster session 2BANQUETWEDNESDAY APRIL 22 8.45 9.25Anne De VernalSea-ice, sea-surface salinity and the halo/thermocline structure in the northern North Atlantic: modern vs. last glacial maximum 9.24 10.05Sylvie JoussaumeThe Paleoclimate Modeling Intercomparison Project: what can we learn when using several different climate models run under past climates? 10.05 10.45Sandy HarrisonHow well can we simulate past climates? Evaluating the models using global paleoenvronmental data setsCoffee break11.15 11.55Jean JouzelWater isotopes in precipitation : Data/model comparison for present-day and past climates 11.55 12.35David RindTBALunch14.00 14.40Colin PrenticeRole of the terrestrial biosphere in Earth system dynamics. 14.40 15.20Ed BoyleAbrupt climate change and the ocean thermohaline circulation: the search for causes and effects 15.20 16.00Tom PedersenInfluences of oceanic rheostats and amplifiers on atmospheric pCO2 during the late quaternary 16.00 18.00 Poster session 3 THURSDAY APRIL 23 8.45 9.25Paul ColinvauxResponse of Amazonian and other tropical plant communities to climatic changes of glacial cycles. 9.25 10.05Rick BattarbeeLakes, climate change and the role of paleolimnology: past changes, future threats 10.05 10.45Peter DeMenocalHolocene variations in subtropical Atlantic Climate and SSTs: a perspective on past social implications of abrupt changeCoffee break11.15 11.55Jonathan OverpeckAssessing future climate change and its impacts: the role of PAGES data 11.55 12.35Bruno MesserliTBALunch14.00 16.00Panel Discussion chaired by Chris Rapley The Poster presentations will be broken into three one day sessions and arranged thematically. The deadline for poster abstract submission is now past. Late poster abstracts are welcomed until March 15th although inclusion in the published abstracts volume cannot be guaranteed. Registration: The deadline for registration is March 15th, with late registrations possible up to the time of the meeting itself with additional fees imposed. Pre-registration forms, housing registration forms, and the latest information on the meeting are available by e-mail from the PAGES office ( or from the PAGES website ( .OPEN SCIENCE MEETING

PAGES (Past Global Changes) supports research aimed at
understanding the Earth's past environment in order to make
predictions for the future. We encourage international and
interdisciplinary collaborations and seek to promote the
involvement of scientists from developing countries in the
global paleo-community discourse.
PAGES scope of interest includes the physical climate
system, biogeochemical cycles, ecosystem processes,
biodiversity, and human dimensions, on different time
scales Pleistocene, Holocene, last millennium and the
recent past.
Founded in 1991, PAGES is a core project of the
International Geosphere-Biosphere Programme (IGBP) and is
funded by the U.S. and Swiss National Science Foundations,
and the National Oceanic and Atmospheric Administration
It is overseen by a Scientific Steering Committee (SSC)
comprised of members chosen to be representative of the
major techniques, disciplines and geographic regions that
contribute to paleoscience.


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