To: LindyBill who wrote (98857 ) 2/6/2005 12:34:57 AM From: Volsi Mimir Respond to of 793886 Hawaii-Isn't it a bit of coincidence that the place where they sample for CO2 and used in all the green house reporting is next to one of most frequently erupting volcanoes? Mauna Loa Observatory on the island of Hawaii and Kilauea: (usgs.gov) The caldera was the site of nearly continuous activity during the 19th century and the early part of this century. Since 1952 there have been 34 eruptions, and since January 1983 eruptive activity has been continuous along the east rift zone. All told, Kilauea ranks among the world's most active volcanoes and may even top the list. and Mauna Loa itself was last active in 1984....... and how come they just don't use the samples from Antartica that is previous to that-(that is usually what I see-- pre-Mauna Loa its the Antartica site. Probably both have a reasonable explanation, I just haven't found one casually looking and reading. or maybe just add iron to the water:(my mother use to tell me that once) Phytoplankton may stimulate uptake of CO2 New research has revealed that phytoplankton may be one of the main historic controls on global warming, and that fertilizing the oceans with iron results in increased phytoplankton productivity – a hypothetical way to offset the effects of global warming. Through photosynthesis, these tiny, free-floating aquatic plants can convert carbon dioxide to organic carbon, and there appears to be a prehistoric relationship between iron in the ocean and atmospheric levels of carbon dioxide. Burke Hales, an assistant professor in the College of Oceanic and Atmospheric Sciences at Oregon State University, is one of a number of scientists who collaborated on a new study which involved field research in the ocean near Antartica and will be published Friday in the journal Science. He described the research as "tremendously successful" because it very clearly shows an induced biological response in the oceans to fertilization with iron. "During the glacial periods, atmospheric carbon dioxide, or CO2 levels decrease substantially, while during interglacial periods, such as we are now in, those levels increase," said Hales. "There is also a striking inverse relationship between implied, historical iron fluxes to the ocean and atmospheric CO2 concentrations. These relationships suggest some sort of feedback system between iron and CO2 levels during glacial periods that keep the temperature low."....morescienceblog.com