AnnualMeeting_Announcement 2015
Transcription
AnnualMeeting_Announcement 2015
Invitation to the 2015 Review Meeting and Field Trip The annual review meeting of the CSL – Center for Carbonate Research will be held September 14-15, 2015 in Miami at the Rosenstiel School of Marine and Atmospheric Science on Virginia Key. During the annual review, we will report the results of the ongoing projects and discuss the planned projects for the coming year. A list of the projects covered during the meeting is listed below and on the website: www.cslmiami.info This year’s fieldtrip (September 15-19, 2015) will be to Eleuthera in the Bahamas with a focus on three topics. The first is the complexity of marginal grainstone belt, which will be examined at the spectacular Pleistocene outcrops of the last interglacial period (MIS 5e) at Glass Window and Boiling Hole area in northern Eleuthera. The second theme is karst that we will inspect in karst holes and in caves where we currently study rates and composition of speleothems. The third topic is the modern ooid shoal formation at Schooners Cay. The cost of the fieldtrip is $4200.-. It includes all transportation in the Bahamas, lodging, meals, field guidebook and gear. Logistics Annual Review Meeting - September 14-15, 2015 The meeting will begin at 8:30 AM on Monday, September 14th in the seminar room at the University of Miami’s Rosenstiel School of Marine & Atmospheric Science (RSMAS), 4600 Rickenbacker Causeway. The seminar room is in the Science/Administration Bldg., Rm. 103 (follow signs). We will not be providing transportation to the meeting. The taxi ride from the hotel to RSMAS is about 15 minutes. The review meeting will end by 1:00 PM on Tuesday, September 15th. Please arrive in Miami by the evening of September 13th. We are reserving a block of rooms for the nights of September 13th & 14th at the University of Miami rate of $139.00 (plus tax) per night for single/double occupancy at the Sonesta Bayfront Hotel Coconut Grove, 2889 McFarlane Rd, Coconut Grove, FL 33133. We have only reserved a block of rooms – you must make your own reservation. You may make your reservation online using the group code: - To book online reservations please go to: https://gc.synxis.com/rez.aspx?Hotel=12604&Chain=5157&arrive=9/13/20 15&depart=9/15/2015&adult=1&child=0&group=0913CSLANN The ‘Group’ code is already entered for you Click ‘check availability’ and choose room/suite type and rates. - If you prefer to call in your reservation; you may do so by calling 1-800SONESTA and: Make reference to the UM - RSMAS - CSL - Annual Review Meeting Guests must let the reservations agent know the Group Code: 0913CSLANN The deadline for making your reservation is Friday, August 28, 2015 before 5:00 PM. After that time, all rooms that have not been reserved will be returned to the hotel’s general inventory and will be accepted on a space and rate available basis. There will be a daily service fee of $5.00 per person, per night, which includes hotel housekeeping and bellman services. This fee is separate and distinct from the room rate and taxes. Accommodations will be available at 3:00 pm on arrival day and reserved until 12:00 pm on departure day. The field trip participants will fly to Eleuthera, Tuesday afternoon, September 15th. A detailed itinerary is given below. Registration Please register for the meeting and the fieldtrip by e-mail or phone as soon as possible with Karen Neher. Her email address is [email protected] and her phone number is (305) 421-4684. By registering for the field trip you agree to pay the field trip fee. It is especially important to make the field trip reservation as soon as possible for our planning purposes. Registration deadline for the fieldtrip is Thursday, July 30, 2015. Registration and hotel deadline for the meeting is Friday, August 28, 2015. We hope to see many of you at the meeting. Best regards, ANNUAL REVIEW TOPICS Unconventional Reservoirs The Vaca Muerta Research Initiative – Neuquén Basin, Argentina Gregor P. Eberli Distal Expression of Source Rock Intervals in the Vaca Muerta Formation Max Tenaglia, Leticia Rodriguez Blanco, Laura E. Rueda, Gregor P. Eberli, and Peter K. Swart Tracing Los Catutos Carbonates within the Vaca Muerta Formation Leticia Rodriguez Blanco, Max Tenaglia, Laura E. Rueda, Gregor P. Eberli, Ralf J. Weger, and Jose L. Massaferro Geochemical and Petrophysical Calibration of Cycles in the Vaca Muerta Formation Laura E. Rueda, Gregor P. Eberli, Max Tenaglia, Leticia Rodriguez Blanco, and Ralf J. Weger Acoustic Properties of Shale-TOC-Limestone Mixtures in the Vaca Muerta Formation Ralf J. Weger, Ergin Karaca, Jan H. Norbisrath, and Gregor P. Eberli Formation and Stratigraphic Position of Marine Concretions in Miocene and Jurassic Mudstone Cycles Donald F. McNeill, Max Tenaglia, Peter K. Swart, Ralf J. Weger, Gregor P. Eberli, and James S. Klaus Carbonate Systems and Reservoir Characterization Accommodation Space on an Isolated Carbonate Platform – Patterns and Implications Sam J. Purkis and Paul M. (Mitch) Harris Timing of the Pleistocene MIS 5e Sea-Level Oscillation and the Holocene Transgression: Evidence from the Bahamas Kelly L. Jackson, Gregor P. Eberli, Paul M. (Mitch) Harris, and Donald F. McNeill, and Ali Pourmand Deciphering the Amplitude of Sea-Level Oscillations and Quantifying the Resultant Heterogeneity of Grainstone Bodies Kelly L. Jackson, Gregor P. Eberli, Paul M. (Mitch) Harris, and Donald F. McNeill Depositional and Diagenetic Evolution of a Fringing Reef during PlioPleistocene Sea-Level Cycles Viviana D. Díaz, James S. Klaus, Donald F. McNeill, Peter K. Swart, and Ali Pourmand Deposition and Early Burial of Holocene Freshwater Carbonates Chelsea L. Pederson, James S. Klaus, Donald F. McNeill, and Peter K. Swart Deep-Water Carbonates off Great Bahama Bank - A MultiInstitutional Research Effort Gregor P. Eberli, Jara S. D. Schnyder, Anna H. Ling, and Kimberly C. Galvez, and Christian Betzler, Thomas Lüdmann, Marco Palaut, and colleagues, and Dierk Hebbeln, Paul Wintersteller, and colleagues, and Thierry Mulder and colleagues Event Stratigraphy in the Straits of Florida Jara S. D. Schnyder, Gregor P. Eberli, Deniz Kula, Christian Betzler, Thomas Lüdmann, Marco Palaut, Sebastian Lindhorst Current Influence on Basin Sedimentation and the Adjacent Carbonate Platforms, Bahamas (year 2) Marco Palaut, Thomas Lüdman, Christian Betzler, Gregor P. Eberli, and Linda Schiebel Timing of Pulses of Cold-water Coral Growth in the Straits of Florida Kimberly C. Galvez, Rani Sianipar, Gregor P. Eberli, Jürgen Titschack, and Dierk Hebbeln Deposition and Erosion at the Florida Shelf Edge Anna Ling, Gregor P. Eberli, Dierk Hebbeln, Claudia Wienberg, Paul Wintersteller, Nicholas Nowald, Götz Ruhland, and Ralf Schiebel Petrophysics and Near-Surface Geophysics Regional GPR & GPS Survey of Downstepping Pleistocene (MIS 5e) Beach Deposits: New Providence Platform, Bahamas Kelly L. Jackson, Mark Grasmueck, Pierpaolo Marchesini, and Gregor P. Eberli Complex Resistivity Spectra in Carbonates and Shales to Estimate Specific Surface Area and Permeability Jan H. Norbisrath, Ralf J. Weger, Gregor P. Eberli, and G. Michael Grammer Rheological Properties of Carbonates in the Context of Depositional Lithology Jara S. D. Schnyder and Ralf J. Weger Geobiology and Microbialites Geo-Microbial Processes in the Fresh-Water–Saltwater Transition Zone of a Reefal Margin James S. Klaus, Donald F. McNeill, Viviana D. Díaz, and Peter K. Swart Challenging the Default Notion of Ooid Formation Mara R Díaz, Peter K. Swart, and Gregor P. Eberli Geochemistry and Diagenesis of Carbonates Clumped Isotopes of Bahamian Dolomites Sean Murray and Peter K. Swart Using Clumped Isotopes to Constrain Diagenetic Temperatures in Oceanic and Periplatform Carbonates Philip T. Staudigel and Peter K. Swart The Changing Mg/Ca Ratio in the Oceans and its Record in Coral Skeletons Sharmila Giri and Peter K. Swart Understanding the Clumped Isotopic Systematics during Meteoric Diagenesis using Speleothem Analogs Sevag S. Mehterian and Peter K. Swart Post Meeting Field Trip: Eleuthera Island, Bahamas September 15/16–19, 2015 Leaders Gregor P. Eberli, Peter K. Swart, Kelly Jackson, Paul M. (Mitch) Harris Rationale and Overview The lateral and vertical heterogeneity in marginal grainstone complexes and ooid shoals is the result of a repeated interplay between physical, chemical and stratigraphic processes. In northern Eleuthera all these processes can be examined in close proximity. The modern ooid shoal of Schooners Cay is a very large tidal bar belt whose size and heterogeneity is largely driven by currents and their interaction with platform margin morphology, antecedent and newly created topography. Early meteoric cementation on Holocene islands and marine cements in the shallow subsurface are the first chemical overprint on these shoals. Sea-level fluctuations produce stacks of grainstone complexes along the platform margin. In Eleuthera two vertically stacked shallowing-upward sequences of oolitic coastal deposits are exposed in spectacular exposures at the windward margin. These two successions of beach facies and eolian deposits were deposited during the last interglacial (MIS 5e) and document the higher sea level compared to today and give further evidence of a sea-level oscillation within MIS 5e. The large amplitude of the Pleistocene sea-level fluctuations repeatedly exposed the platform top. Thus, karst features and meteoric diagenesis are ubiquitous in the Pleistocene strata. The size and dimensions of sinkholes and their connectivity to horizontal caves are illustrated by visiting two sinkholes. Flank margin caves are common in carbonate eolian grainstones. A well accessible cave in Eleuthera is the study site for geochemical experiments by the CSL where speleothems are used for the study of clumped isotopes and fluid inclusions. We will visit this site to illustrate the formation and typical size of these bank margin caves and to demonstrate the ongoing geochemical study. Logistics Travel: Participants fly to Nassau, Bahamas, on Tuesday afternoon, September 15 and stay overnight in Nassau. In the morning we will fly to Eleuthera. Participants are responsible for booking their own roundtrip ticket from Miami to Nassau. We recommend the following flights: Miami to Nassau: September 15: Bahamas Air #228, Departs Miami 4:40 PM, in Nassau 5:40 PM Nassau to Miami: September 19: Bahamas Air #229 Departs Nassau 7:00 PM, in Miami 7:55 PM There are limited flights to and from Eleuthera. Returning, we will arrive in Nassau around 3:00 PM on September 19. You will clear U.S. customs in Nassau before departing for the U.S.; therefore, please allow time for this before your outgoing flight. Cost: The field trip begins and ends in Nassau. The cost is $4,200.-. This includes round-trip flights from Nassau to Eleuthera, ground transportation, boat in Eleuthera, hotel accommodations in Nassau (night of September 15) and Eleuthera, meals, and course notes. Not included in the fieldtrip costs are the flights to and from Nassau. Registration: Please register as soon as possible but no later than July 30, 2015 by sending an email to [email protected] and a copy to [email protected] Itinerary and Field Trip Stops Tuesday, September 15 PM Flight to Nassau Wednesday, September 16 AM Flight from Nassau to Eleuthera Transfer from airport to Hotel Sky Beach Club, Eleuthera Introduction to the field trip and safety briefing PM Karst: Caves and sinkholes Main focus: Formation and distribution of sinkholes and flank margin caves. Stops include: • Cave in southern Eleuthera • Ocean Hole, Rock Sound • Big Pond: Microbially mediated precipitation in a hypersaline lake Thursday, September 17 Schooners Cay: Facies and geometries of the tidal bars within the Schooners Cay ooid shoal Main focus: Formation, size and distribution of the tidal bars in relation to platform morphology and tidal energy. Stops include: • Holocene island with beach rock • Intertidal bar • Subtidal channels Friday, September 18 Stratigraphic complexity of marginal grainstones deposited during the last interglacial: Glass Window and Boiling Point Main focus: 1) Stratigraphic heterogeneity of marginal grainstone bodies, 2) Erosional processes at the windward margin, 3) Size and distribution of marginal grainstone complex. Stops include: • Glass Window: grainstone bodies separated by exposure horizons; sea ward erosion • Boiling Point: Examination of the two beach/eolian successions deposited during the last interglacial and the implication for vertical heterogeneity and fluid flow units • Bight of Eleuthera: Cow and Bull boulders erosional remnants of eolian dunes Saturday, September 19 AM The Holocene transgression and modern eolian formation Main focus: Erosional processes along the windward bank margin during the Holocene sea level rise. Stops include: • Lighthouse beach PM Return to Nassau and Miami
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