From PHrank2139 at aol.com Tue Dec 5 06:49:17 1995 From: PHrank2139 at aol.com (PHrank2139 at aol.com) Date: Tue, 5 Dec 1995 06:49:17 -0500 Subject: CAUZ network Message-ID: <951205064916_125365004@emout05.mail.aol.com> FORWARDED MESSAGE The Consortium of Aquariums, Universities and Zoos [C.A.U.Z. for Worldwide Conservation] This international network was formed ten years ago in response to the perceived need to facilitate communication between university scientists and educators and their counterparts in zoos and aquariums. While many people at these institutions have shared interests and may even be studying the same species, the sharing of data and collaboration on projects between university scientists and zoo/aquarium professionals has been relatively rare, especially when their institutions are in different countries. Those who become part of the C.A.U.Z. Network share information on their interests in specific taxonomic groups (e.g., Order Sphenisciformes), their general interests (e.g., penguin ecology), and their current projects (e.g., field studies of the Humboldt penguin). Information from the C.A.U.Z. database is published in annual directories and also appears on its site on the World-Wide Web: http://www.fhcrc.org/~ialwww/CAUZ/CAUZ.html This database is a searchable online. A keyword search for "penguin" can find Ed Diebold, the Director of Animal Collections at the Riverbanks Zoological Park in Columbia, South Carolina, who studies Humboldt penguins in Chile. Ed is also involved in trumpeter swan recovery and piping plover egg rescue and is part of organized zoo efforts in the captive propagation of raptors. Keyword searches also reveal addresses, phone and fax numbers and email addresses (if available). [Email addresses in the C.A.U.Z. database are "hot" so that one can contact a person by email with a "mouse click" without leaving our Web Site.] Collaborations made possible by the C.A.U.Z. Network can contribute greatly to international conservation initiatives. Those involved in wildlife research and conservation, restoration ecology, captive propagation of endangered species, wildlife rehabilitation and reintroduction, and veterinary medicine (esp. with exotic species) who wish to become part of the C.A.U.Z. Network can contact its Coordinator: Donna FitzRoy Hardy, Ph.D. Professor of Psychology California State Univ., Northridge Northridge, California 91330 USA Phone:(818) 885-4970 (or 885-2827 for messages) Fax: (818) 885-2829 Email: dhardy at huey.csun.edu C.A.U.Z. Web Site: http://www.fhcrc.org/~ialwww/CAUZ/CAUZ.html From gregorh at hk.super.net Wed Dec 6 08:52:15 1995 From: gregorh at hk.super.net (gregorh at hk.super.net) Date: Wed, 6 Dec 1995 21:52:15 +0800 (HKT) Subject: Vacancies Message-ID: <199512061352.VAA20768@is1.hk.super.net> Date: Sat, 2 Dec 1995 00:50:32 -0500 From: PUISHAN at aol.com Subject: Vacancies I am writing with a request for suitable personnel for the following two posts for UNDP: =0D 1) A "Media Advisor" to work in Cambodia for 11 months for the 3 year ET= AP - Environmental Technical Assistance Programme". His/Her main duty will be= to assist the Government and NGOs to develop environmental education / publi= c awareness promotional materials; mainly TV programmes, films, radio shows= , performances, etc. The person should have a degree & experience in relat= ed fields & preferably work experience in Asia. UNOPS - Office of Project Services is trying very hard to find somebody to begin the job in January= =2E = =0D 2) A "Marine Expert" for a regional project for Vietnam, Cambodia, Thail= and and Laos. The project had a major terrestrial component, the key objectiv= e of which is to promote regional cooperations in nature conservation; involvi= ng transboundary protected areas, regional dialogue/networking, cooperation = in research, training, etc. The Marine Expert will be given a short contrac= t of 3 months to initiate dialogue among the countries and recommend possible cooperations. Biodiversity hotspot areas will be identified through consultation with existing literature and national experts; except for Cambodia where marine studies are especially limited and hence will necessitate some field assessment. The person should hold a M.Sc degree = (or higher) on marine sciences & be experienced in marine conservation, prote= cted areas, policies, and preferably with work experience in the project countries. = =0D I would be really grateful if you could spread the word around and assist= us find potential candidates for the above two projects. If you do find an interesting party, please give him/her my email address puishan at aol.com = or ask them to write directly to: =0D Mr Roger Aertgeerts Senior Project Management Officer UNOPS Fax: 1-212-906 6501 Em: roger.aertgeerts at undp.org =0D Many thanks & regards, Catherine Cheung RBAS, UNDP =0D = --PART.BOUNDARY.0.27553.mail04.mail.aol.com.817883427-- <---- End Included Message ----> From Geok.Koh at jcu.edu.au Thu Dec 7 20:13:01 1995 From: Geok.Koh at jcu.edu.au (Esther Koh) Date: Fri, 8 Dec 1995 11:13:01 +1000 (EST) Subject: Mark Erdmann's contact In-Reply-To: Message-ID: Herman, > First, I am trying to contact Mark Erdmann who has done some very > interesting work on coral reef ecology. Does anyone know his e-mail or > other address? I have Mark's contact details. Please email me. Esther G.L. Koh Department of Marine Biology James Cook University of North Queensland Townsville, Q4811 AUSTRALIA Tel: 61-77-814801 Fax: 61-77-251570 From 3rel1 at qlink.queensu.ca Wed Dec 13 16:38:10 1995 From: 3rel1 at qlink.queensu.ca (Lamond Robert E) Date: Wed, 13 Dec 1995 16:38:10 -0500 (EST) Subject: Graduate research on coral-reefs. Message-ID: Hello. I am a fourth year undergraduate student, searching for a potential university to study and conduct graduate level reasearch on Modern Coral Reefs. I will be graduating with a BscH in Geology from Queen's University, Canada this April. I have been specializing in carbonate sedimentology and invertebrate paleontology at Queen's and I am searching for a graduate program on reef geology/ biology. If anyone has knowledge of such a program, or has an address I might contact for more information, please e-mail me at 3rel1 at qlink.queensu.ca. The nationality of the university is not as important as the proximity to the reefs! Thank you for your time, Bob Lamond From j.reichman at mail.utexas.edu Fri Dec 15 00:17:22 1995 From: j.reichman at mail.utexas.edu (JAY RANDALL REICHMAN) Date: Thu, 14 Dec 1995 23:17:22 -0600 Subject: Email Internet Virus Message-ID: <199512150517.XAA11525@mail.utexas.edu> >Date: Thu, 14 Dec 1995 22:55:02 -0600 >To: JLBrown68 at aol.com >From: khaywood at mail.utexas.edu (Keene M. Haywood) >Subject: Email Internet Virus >Cc: belflite at orion.ae.utexas.edu, bosque at mail.utexas.edu, > dolitl at mail.utexas.edu, pmiller at nwu.edu, YGHQ78D at prodigy.com, > CCORNELI at WINNIE.FIT.EDU, SSeaFresh at aol.com, Narragan at aol.com, > cstinson at mail.utexas.edu, kkishi at maestro.geo.utexas.edu, > armentrc at ava.bcc.orst.edu, iomarine at tiac.net, waiblee at ucs.orst.edu, > imanners at uts.cc.utexas.edu, ICLARM at CGNET.COM, > J.Reichman at mail.utexas.edu, JeffM4079615 at eworld.com, > jc690254 at bcm.tmc.edu, jgifford at rsmas.miami.edu, KB78 at COLUMBIA.EDU, > k.foote at mail.utexas.edu, VonWestarp at aol.com, M.GOROSPE at CGNET.COM, > SPATZY at aol.com, MQUETEL at TELEPORT.COM, NHay5600 at aol.com, > nfowler at spice.cc.utexas.edu, drbob at mail.utexas.edu, > rdoughty at mail.utexas.edu, roshanr at mail.utexas.edu, chocolat at eden.com, > cshane at ccwf.cc.utexas.edu, DFLIGHT at HOOKED.NET, linscott at rice.edu, > swells at ucb.edu.bz, tthys at acpub.duke.edu, dlarson340 at aol.com > >>>>Mail*Link(r) SMTP FWD>Internet Virus Warning!!! >>>> >>>>>There is a computer virus that is being sent across the Internet. If you >>>>>receive an e-mail message with the subject line "Good Times", DO NOT read >>>>the >>>>>message, DELETE it immediately. Please read the messages below. Some >>>>>miscreant is sending e-mail under the title "good times" world-wide. If you >>>>>get anything like this, DON'T DOWN LOAD THE FILE! It has a virus that >>>>>rewrites your hard drive, obliterating anything on it. Please be careful and >>>>>forward this mail -- I have. >>>> >>>>WARNING!!!!!!!!!: INTERNET VIRUS >>>>The FCC released a warning last Wednesday concerning a matter of major >>>>importance to any regular user of the Internet. Apparently, a new computer >>>>virus has been engineered by a user of America Online that is unparalleled >>>>in its destructive capability. Other, more well-known viruses such as >>>>Stoned, Airwolf, and Michaelangelo pale in comparison to the prospects of >>>>this newest creation by a warped mentality. What makes this virus so >>>>terrifying, said the FCC, is the fact that no program needs to be exchanged >>>>for a new computer to be infected. It can be spread through the existing >>>>e-mail systems of the Internet. Once a computer is infected, one of several >>>>things can happen. If the computer contains a hard drive it will be >>>>destroyed. If the program is not stopped, >>>>the computer's processor will be placed in an nth-complexity infinite binary >>>>loop -which can severely damage the processor if left running that way too >>>>long. >>>>Unfortunately, most novice computer users will not realize what is >>>>happening until it is far too late. Luckily, there is one sure means of >>>>detecting what is now known as the Good Times" virus. It always travels to >>>>new computers the same way in a text e-mail message with the subject line >>>>reading simply "Good Times". Avoiding infection is easy once the file has >>>>been received - not reading it. The act of loading the file into the mail >>>>server's ASCII buffer causes the "Good Times" mainline program to >>>>initialize and execute. The program is highly intelligent - it will send >>>>copies of itself to everyone whose e-mail address is contained in a >>>>received-mail file or a sent- mail file, if it can find one. It will then >>>>proceed to trash the computer it is running on. The bottom line here is- >>>>if you receive a file with the subject line "Good Times", delete it >>>>immediately! Do not read it! Rest assured that whoever's name was on the >>>>"From:" line was surely struck by the virus. Warn your friends and local >>>>system users of this newest threat to the Internet! >>>> >>>> >>>> >>>> >>> >>> >> >> > > > Adios, Jay Reichman Department of Zoology University of Texas at Austin From pdh at u.washington.edu Fri Dec 15 02:15:48 1995 From: pdh at u.washington.edu (Preston Hardison) Date: Thu, 14 Dec 1995 23:15:48 -0800 (PST) Subject: Email Internet Virus In-Reply-To: <199512150517.XAA11525@mail.utexas.edu> Message-ID: The only pathogen here is the "Goodtimes Virus Alert". This hoary old cyber-legend has been circulating around the Internet for three or four years now, and is well known to be a junk alert. There simply is no danger from a "Good Times" ascii file. You can get a virus from a program embedded as a binary attachment to an email message, but only after you have downloaded the file and executed it on your PC. Merely reading an email message will not cause harm to your computer. If someone knows otherwise, please supply an authoritative reference (the reference to the "FCC" in the alert is bogus). Please don't forward the alert on to other lists. Preston Hardison pdh at u.washington.edu From jogden at jaws.marine.usf.edu Fri Dec 15 11:13:49 1995 From: jogden at jaws.marine.usf.edu (John Ogden) Date: Fri, 15 Dec 1995 11:13:49 -0500 (EST) Subject: FKNMS Management Plan Message-ID: The following Open Letter sent to the Miami Herald and the Key West Citizen is FYI. December 14, 1995 An Open Letter to the Commercial Fishermen of the Florida Keys: As most of you know, this week the Sanctuary Advisory Council (SAC) of the Florida Keys National Marine Sanctuary finished its task of reviewing the 10 Action Plans which form the Management Plan of the Florida Keys National Marine Sanctuary. These were revised over the past year in a series of community meetings led by SAC members. The Plan approved by the Council on December 12 will help to insure that the fragile marine environment of the Keys will sustain and enrich the lives of future generations. The approved Plan is the culmination of 4 years of effort on the part of the SAC members who worked hard to integrate the interests and concerns of their various constituencies in a complicated, controversial, and politically-charged task. Fishermen's interests were ably represented by Tony Iarocci, Michael Laudicina, SAC Chair Michael Collins, and by the many fishermen who took valuable time away from their businesses to attend hearings and meetings and to testify in a constructive manner on the plan. In fact, it is fair to say that fishermen, more than any other constituency, defined the Management Plan that we all hope will be signed by the Governor at the end of 1996. However, in my opinion the virtual elimination of the Replenishment Reserves by the organized, disciplined, and effective campaign against them seriously compromises the intent of the plan to sustain the harvest of fisheries resources in the future. We need at least three relatively small, representative Replenishment Reserves strategically placed in the Upper and Lower Keys and in the Dry Tortugas. The approved plan eliminated the Upper Keys Reserve and left the one in the Dry Tortugas in limbo waiting action by the National Park Service. There is only one effective Reserve, a sliver of habitat from shore to the reef edge in the Sambos. The Reserves are critical to gather baseline data from undisturbed, unharvested areas so we can assess the impact of harvest and disturbance in the rest of the Sanctuary. Reserves are also an experiment, one that the world is watching, to see if small, strategically placed unharvested areas can provide "replenishment" to the harvested resources outside its boundaries. There is a scientific consensus that the Reserves will work, and there are examples of early success from other countries including New Zealand, Australia, Kenya, and many Caribbean nations. You don't have to be told that the Keys fishery resources are vulnerable; fishermen have seen this from yearly catches. What may not be well known is that reefs appear to be particularly sensitive to the removal of the large size classes of snappers and groupers as well as parrotfishes. This disrupts the balance of the reef and leads to elimination of corals and to dominance of the reefs by algae. This is a condition that we are seeing nearly everywhere in the Keys. The Replenishment Reserves are the only tool that we have to assess these impacts and to define strategies that will sustain the fisheries harvest. I ask each of you to reconsider your position with respect to the Replenishment Reserves. Talk with each other and with your leaders and work with NOAA to place at least three Reserves in the Sanctuary-- one in each of the major representative habitats of the Keys. If this is accomplished we can continue the cooperative interaction among the fishing industry, management agencies, and the science community that has given us a remarkable and exemplary Management Plan for the marine resources of the Keys. Thank you for your consideration, congratulations on your very effective and informative work, and Season's Greetings to all. Sincerely, John C. Ogden Member SAC for Science John C. Ogden Director Phone: 813/893-9100 Florida Institute of Oceanography Fax: 813/893-9109 830 First Street South St. Petersburg, Florida 33701 From gheiss at geomar.de Fri Dec 15 11:02:19 1995 From: gheiss at geomar.de (Georg Heiss) Date: Fri, 15 Dec 1995 17:02:19 +0100 Subject: Research programme on coral reefs in the Western Indian Ocean Message-ID: Dear colleagues, With this message we would like to spread information about a current research programme on recent and fossil coral reefs in the Western Indian Ocean. If you would like to have more detailed information, please contact any of the members of the group at the addresses listed at the end of this message. At the moment we are constructing a WWW-page with more information about the activities of the group. As soon as we are online, you will be informed via the coral-list. Georg Heiss _________________________________________________ CORAL AND REEF GROWTH IN THE WESTERN INDIAN OCEAN: PALEOCLIMATIC IMPLICATIONS INTRODUCTION Since 1994 a group of European reef geologists including workers from France, Germany, Italy and the U.K. has been investigating Western Indian Ocean reefs, studying paleoclimatology and sea-level changes. These studies comprise localities over a latitudinal range between 4 degrees and 23 degrees south, spanning in the north the Seychelles Bank, Aldabra-Atoll, and Mayotte (Comoro Islands), and in the south,Tulear (Madagascar), Reunion and Mauritius. The approach is on three time scales using: 1. Living corals to document coral growth and climatic change over the last 1000 years. 2. Drill cores in Holocene reefs to cover the last 10,000 years. 3. Outcrops of Pleistocene limestones to investigate the past 130,000 years and including: a) Sampling of raised Eemian limestones; b) Studies of drowned reef terraces (isotope stage 3 and LGM, 20-18 ka) by submersible. CORAL CORES Cores collected from massive coral colonies (Porites) allow the determination of growth bands and of an exact chronology, together with the vertical accretion rate of the colony and variations in stable isotopes of O and C, and of Sr with high temporal resolution. The delta 18O-composition of the skeletal aragonite is used as a proxy for both paleotemperature and salinity. In general, a variation of 0.22 permil is equivalent to 1 degree C of temperature change (Epstein et al. 1953) but is also linked to evaporation and precipitation (Swart and Coleman 1980). The delta 13C-composition serves as a proxy for both the biological productivity of the coral and the CO2 content of the contemporary atmosphere (Nozaki et al. 1978). Tropical sea surface palaeotemperatures can also be determined with high precision by means of Sr/Ca-TIMS (thermal ionization mass spectrometry), producing a seasonal resolution over at least the past 10,000 years (Beck et al. 1992). This method promises to provide an additional independent means of determining temperature which is probably less influenced by fluctuations in the volume of ice-caps and oxygen isotope variations or by evaporation or freshwater influx (Beck et al. 1992; De Villiers et al. 1994). The isotopic compositions of the skeleton forming the youngest parts of the coral cores can be calibrated with temperature readings from automatic temperature loggers. These have been installed for two years at some of the sampled colonies and provide measurements over this time span in steps of 2 hours. Sampling of coral slabs with computerized drill equipment (sampling in steps of 1/100 mm) theoretically allows the determination of up to 100 samples per year. For these studies we sample in steps of 1 mm, resulting in a resolution of ca. 8-16 samples per year of coral growth, depending on the relative growth rates of the corals. Samples available from recent Porites-colonies are summarized in Table 1. ________________________________________________________ TABLE 1: RECENT CORAL CORE SAMPLES LOCATION__NO. OF CORES__LENGTH OF LONGEST CORE__WATER DEPTH RANGE__DATE of FIELD WORK Mayotte, Comoros___10___238cm__1 to 7m__March 1994 Seychelles__10__203cm__2 to 9m__October 1994, November 1995 Reunion__6__195cm__6 to 13m__October 1994, November 1995 Tulear, Madagascar__16__404cm__0.5 to 7m__October 1995 ________________________________________________________ HOLOCENE DRILL CORES Methods The Holocene reefs have all been drilled close to their outer edges in order to obtain the maximum thickness of the carbonate deposited during the Holocene. Corals and associated organisms (e.g. algae, molluscs) occurring within the cores will be identified to species level in order to evaluate the palaeobathymetry. Age determinations based on U/Th-TIMS may then provide a dataset for establishing a sea level curve. Information can also be gained on the relative rate of reef growth and its response to sea level change, either 'keep up' or 'catch up' styles. Core material will also be examined petrographically to determine both the degree and style of diagenetic alteration. Larger coral colonies recovered will be investigated using the same methods applied to the recent coral cores. This will provide short sclerochronological datasets which will include paleotemperature variability on a sub-annual resolution for different time intervals during the Holocene. Both the general environmental parameters and the specific patterns of change which these reveal will be compared with those of the recent corals. Locations The group has recovered cores from Reunion, Mauritius and Mayotte in recent years, and drilling operations have been completed at Tulear and on Mahe in the Seychelles this year. On average, Holocene carbonates are more than 20m thick in the Western Indian Ocean. The oldest Holocene corals collected so far are from Mayotte and have been dated at 9,800 yrs B.P. (Colonna 1994). The underlying substratum varies with the origin and age of the islands. In Reunion, the basement is probably formed by Pleistocene basalts, while in Mayotte and Mauritius the Holocene reef sequences overlie Pleistocene limestones. On Mahe they rest on what are probably terrestrial silts and clays which themselves overlie Precambrian granite. EEMIAN RAISED LIMESTONES Methods Large EemianPorites-heads have been sampled and are being analyzed using methods identical to those applied to the recent samples (sclerochronology, stable isotopes). Petrographic studies are being carried out on material from the same outcrops to assess the degree of alteration. The ages of these carbonates will be determined using U/Th dating. Locations Outcrops of Eemian limestone terraces are exposed on the Seychelles Islands, principally in small outcrops beneath granite boulders (Mahe) but including thick (metres) in situ algal and coral crusts on Praslin and La Digue. More extensive outcrops are found on Aldabra and other so-called 'high' limestone islands to the west. Detailed stratigraphical data are available for Aldabra, Kenya, Madagascar, Mauritius and Reunion from earlier studies by the group. Additional data The group also has a sample set collected during a German-French mission to Mayotte using the research submersible "Jago". During this mission several coral samples and reef rock samples were recovered. It has been shown that reefs flourished during isotope stage 3 (50 - 27 ka B.P.) forming extended terraces presently drowned to around 80 m deep. Last glacial maximum (LGM) corals were also collected, giving hints of a maximum sea level fall of 150 m for the volcanic island of Mayotte. Such extreme values seem to be typical for volcanic islands having no gravity differential with the ocean crust and therefore providing a regional hydroeustacy (Peltier 1991; Lambeck and Nakada 1992). FUNDING The studies are financed by a variety of funding agencies. The European Union Programme "TESTREEF" (TEmporal and Spatial Variability in Western Indian Ocean REEFs) is funding the research in Tulear and Seychelles. Investigations on Reunion and Mayotte is funded by PNRCO (Programme National Recifs Coralliens- C.N.R.S.), and by the Deutsche Forschungsgemeinschaft (DFG Du 129/6 and Du 129/9). LITERATURE Beck, J.W., Edwards, R.L., Ito, E., Taylor, F.W., Recy, J., Rougerie, F., Joannot, P. and Henin, C. (1992): Sea-surface temperature from coral skeletal Strontium/Calcium ratios.- Science, 257: 644-647. Colonna, M. (1994): Chronologie des variation du niveau marins au cours du dernier cycle climatique (0-140 000 ans) dans la partie sud occidental de l'Ocean Indien. Implications paleoclimatiques et paleoceanographiques. Ph.D. thesis, Aix-Marseille: 1-303. De Villiers, S., Shen, G.T. and Nelson, B.K. (1994): The Sr/Ca-temperature relationship in coralline aragonite: Influence of variability in (Sr/Ca)seawater and skeletal growth parameters.- Geochimica et Cosmochimica Acta, 58: 197-208. Epstein, S., Buchsbaum, R., Lowenstam, H.A. and Urey, H.C. (1953): Revised carbonate-water isotopic temperature scale.- Geological Society of America Bulletin, 64: 1315-1326. Lambeck, K. and Nakada, M. (1992): Constraints on the age and duration of the age and duration of the last interglacial period and on sea-level variations.- Nature, 357: 125-128. Nozaki, Y., Rye, D.M., Turekian, K.K. and Dodge, R.E. (1978): A 200 year record of Carbon-13 and Carbon-14 variations in a Bermuda coral.- Geophysical Research Letters, 5/10: 825-827. Peltier, W.R. (1991): The ICE-3G model of Late Pleistocene deglaciation: construction, verification and applications.- In: Sabadini, R. (ed.) Glacial Isostacy, Sea Level and Mantle Rheology: 95-119 . Swart, P.K. and Coleman, M.L. (1980): Isotopic data for scleractinian corals explain their paleotemperature uncertainties.- Nature, 283: 557-559. _______________ Adresses of the group members: Colin Braithwaite Lilybank Gardens Glasgow G1 2 8QQ Tel. +44.141.339.8855. Ext. 5449. Fax. +44.141.330.4817 cjrb at geology.gla.ac.uk Gilbert F. Camoin URA 1208 CNRS Universite de Provence Centre de Sedimentologie et Paleontologie 3 Place V. Hugo F-13331 Marseille cedex 3 Tel. +33.91106723 Fax. +33.91649964 gcamoin at cerege.fr (by January 96) Wolf-Christian Dullo GEOMAR Research Center for Marine Geosciences Wischhofstr. 1-3, Geb. 4 D-24148 Kiel Germany Tel +49-431-7202200 Fax +49-431-725391 cdullo at geomar.de Georg A. Heiss GEOMAR Research Center for Marine Geosciences Wischhofstr. 1-3, Geb. 4 D-24148 Kiel Germany Tel +49-431-7202209 Fax +49-431-725391 gheiss at geomar.de Lucien Montaggioni URA 1208 CNRS Universite de Provence Centre de Sedimentologie et Paleontologie 3 Place V. Hugo F-13331 Marseille cedex 3 Tel. +33.91106324 Fax. +33.91649964 Marco Taviani Istituto di Geologia Marina Via Zamboni, 65 I-40127 Bologna Italia Tel. +39-51-244044 Fax +39-51-243117 taviani at boigm2.igm.bo.cnr.it Bernard A. Thomassin Centre D'Oceanologie de Marseille (O.S.U.) Unite associee au CNRS (UA 41) Rue Batterie des Lions F-13007 Marseille Tel. +33-91041617 Fax +33-91041635 thomassi at com.univ-mrs.fr From osp066 at sos.bangor.ac.uk Mon Dec 18 13:51:01 1995 From: osp066 at sos.bangor.ac.uk (PETER COLLINSON) Date: Mon, 18 Dec 1995 18:51:01 +0000 (GMT) Subject: rejoinders In-Reply-To: Message-ID: Hello I am trying to get in contact members of the coral research team in Singapore Are you out there? If so could you please contact me, regarding coral reef research. Many Thanks Peter R J Collinson The University of Hong Kong From coral at coral.AOML.ERL.GOV Fri Dec 8 14:28:31 1995 From: coral at coral.AOML.ERL.GOV (Coral Health and Monitoring Program) Date: Thu, 21 Dec 1995 07:28:31 +30000 Subject: Shutdown...again. Message-ID: Seasons Greetings, Colleagues! Because of the U.S. Government budget negotiations impasse, some or all of the Coral Health and Monitoring services (e.g., list-server, Web page, daily posting of C-MAN data) may be temporarily discontinued. The host machines will remain on, but if something breaks, there will be no one around to fix it. I hope you all have a Merry Chistmas and a Happy New Year! Sincerely yours, Jim Hendee ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ | | | Coral Health and Monitoring Program | | Ocean Chemistry Division | | Atlantic Oceanographic and Meteorlogical Laboratories | | National Oceanic and Atmospheric Administration | | Miami, Florida | | USA | | | | Email: coral at coral.aoml.noaa.gov | | World-Wide Web: http://coral.aoml.noaa.gov | | | ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ From carlson at soest.hawaii.edu Sun Dec 24 21:03:57 1995 From: carlson at soest.hawaii.edu (Bruce Carlson) Date: Sun, 24 Dec 1995 16:03:57 -1000 (HST) Subject: Coral spawning - Solomon Islands In-Reply-To: Message-ID: Solomon Islands: New Georgia group, Minjanga Is., December 11, 1995, ca. 1830 hrs ("twilight"). Various mussid corals (Acanthastrea, Lobophyllia, and Symphyllia) were observed spawning. Aggregations of fishes feeding on the eggs indicated the location of spawning colonies. Large Plectorhinchus ("sweetlips") sucked up the spawn as quickly as it was expelled. One large anemone, Stichodactyla mertensii, also spawned at the same time. Video tape of the spawning was taken for the record. On the following evening at the same time at Matiu Island, more agariciid corals spawned. No acroporids or other groups of corals spawned on either night despite observations which continued until about 2100 hours. Bruce Carlson Waikiki Aquarium University of Hawaii From dafnaz at post.tau.ac.il Tue Dec 26 11:32:48 1995 From: dafnaz at post.tau.ac.il (zeevi dafna) Date: Tue, 26 Dec 1995 18:32:48 +0200 (IST) Subject: Reaserch- assistance Message-ID: To all interested... I'm a student to Marine biology in Tel-Aviv university.I'm writing my tesis now to te M.A degree which I'm going to finish in about a month.My reaserch was on the biology and ecology of a soft coral from the Red-Sea. I'm interesed in working as a research assistent in a rsearch that involves ecology and molecular biology in Marine animals (doesn't have to be corals!).I will be avalable from March 96 until September 96. messages to: Dafna Zeevi. From coral at coral.AOML.ERL.GOV Thu Dec 14 17:42:59 1995 From: coral at coral.AOML.ERL.GOV (Coral Health and Monitoring Program) Date: Wed, 27 Dec 1995 10:42:59 +30000 Subject: Injection Wells in West Maui Message-ID: The following message is being forwarded herewith to the list: Date: Tue, 26 Dec 1995 15:09:35 -0500 From: Ursula Keuper-Bennett To: owner-coral-list at reef.aoml.erl.gov Hello. I have just received word that the EPA (Region 9) has changed its mind yet again about the addition of more injection wells in West Maui. This area of ocean has undergone dramatic decline since 1989 when it experienced its first of several algae blooms. I will once again give videotaped testimony against granting a permit for these wells. In preparation for this it would be very helpful to know of other sites where injection wells or sewage effluent has resulted in eutrophication. I would be especially interested in any areas where Cladophora was the main algae nuisance. I also believe that eutrophication may be a factor in fibropapillomas, a disease of green sea turtles. That is why I am presently frantic to stop these injection wells. The sewage treatment plant in the area dumps the waste directly into the ground. It is within 500 metres of the ocean and they pretend it doesn't go into the ocean. Yet all indications are that many of the corals have died, the area experiences annual algae blooms and 75% of the turtles seen are diseased. 90% of turtles resident to the area are sick. If this has piqued anyone's curiosity, more information about this area and its special environmental problems can be accessed directly at http://www.io.org:80/~bunrab/tumoursa.htm Any help would be appreciated. ^ Ursula Keuper-Bennett 0 0 Mississauga, Ontario /V^\ I I /^V\ Email: howzit at io.org /V Turtle Trax V\ /V Forever Green V\ http://www.io.org/~bunrab From coral at coral.AOML.ERL.GOV Tue Dec 26 17:12:11 1995 From: coral at coral.AOML.ERL.GOV (Coral Health and Monitoring Program) Date: Mon, 8 Jan 1996 10:12:11 +30000 Subject: Injection Wells in West Maui (fwd) Message-ID: The following is a message from Ed Parnell of University of Hawaii, and is herewith forwarded to the list. Sorry for the delay in posting, brought about by the U.S. Government budget impasse. In the future, any messages sent to coral-list at reef.aoml.noaa.gov will be automatically forwarded to the list without need for human intervention (we hope!). JCH ---------- Forwarded message ---------- Date: Thu, 28 Dec 1995 10:22:44 -1000 (HST) From: Ed Parnell To: Coral Health and Monitoring Program Subject: Re: Injection Wells in West Maui Deb Schulman and Ed Laws in the oceanography dept. at UH found that ammonia, nitrate, silicate (indicator of freshwater), and del N-15 ratios were higher at Barbers Point and Ewa Beach than most other areas of Mamala Bay. They implicated cesspools to account for the high ammonia and/or groundwater intrusion from the Ewa plain (cultivated for sugar cane for the last 100 years) to account for the other high variables. The pattern of higher nutrients and del N-15 was robust over the ranges of seasonal variation they observed. This work was part of the Mamala Bay study. Brad Gould, in a separate study within the MBS, found that nitrate concentrations were significantly correlated with wave energy. The relationship was non-linear; nitrate concentrations increased with increasing wave energy, and the slope at which nitrate concentrations increased became steeper with increasing wave energy. Pore waters (including groundwater) are pumped by increasing wave energy. This all means that groundwater is a likely significant source of nitrate. Algal diversity and biomass was quantified as part of MBS by Alison Kay et al. They studied three areas; 1) the natatorium (Waikiki) 2) Sand Isalnd and 3) Honouliuli. Algae were studied at three depths 7, 17, and 27 m during winter 94, summer 94, and winter 95. Temporal and spatial variability of dry weight data was so great, just by looking at their graphs (no stats done unfortunately), that no clear pattern emerged. Algal diversity (as # of genera; no diversity indeces were calculated) was highest at Barbers Point. Lynbia and Pterocladia were dominants at all three sites. From coral at coral.AOML.ERL.GOV Tue Dec 26 17:13:25 1995 From: coral at coral.AOML.ERL.GOV (Coral Health and Monitoring Program) Date: Mon, 8 Jan 1996 10:13:25 +30000 Subject: Injection Wells in West Maui (fwd) Message-ID: Another forwarded message... ---------- Forwarded message ---------- Date: 2 Jan 1996 12:43:17 -0500 From: Haskell, B. To: Coral Health and Monitoring Program Subject: RE: Injection Wells in West Maui FYI, the Florida environmental regulatory commission recently decided not to permit anymore injection wells in the Florida Keys due to nearshore water quality degradation. bhaskell at ocean.nos.noaa.gov From coral at coral.AOML.ERL.GOV Tue Dec 26 17:14:37 1995 From: coral at coral.AOML.ERL.GOV (Coral Health and Monitoring Program) Date: Mon, 8 Jan 1996 10:14:37 +30000 Subject: Injection Wells in West Maui (fwd) Message-ID: This forwarded message is apparently in response to the message posted by Ursula Keuper-Bennett (howzit at io.org). ---------- Forwarded message ---------- Date: Thu, 4 Jan 1996 17:13:31 -0700 From: Jack Hardy To: Coral Health and Monitoring Program Subject: Re: Injection Wells in West Maui Send me your mailing address and I'll send copies of a couple of papers we did years ago on eutrophication along the coast of Lebanon, including algal; blooms. Jack Hardy, Director Center for Environmental Sciences Western Washington University Bellingham, WA 98225-9181 voice 360-650-6108 fax 360-650-7284