Goldschmidt in California meant a drive instead of a flight. The route from Pasadena to Sacramento lead us through the Central Valley of California. While living in greater LA we have been well aware of the drought going on in this state, it was still quite sad to see the many fields transformed into desert, and almond plantations dead and cut down. We also saw the thermometer steadily go up to a balmy 43 °C.
Monday was mostly a day of talks on the solar system. Starting off with Andrew Westphal talking about fluffy interstellar particles, and Meenakshi Wadhwa showing that the Solar System originated in an active star forming region, it was very interesting to learn about the latest science coming from the Curiosity Mars Rover, during the plenary by Pamela Conrad. David Blake had a great follow-up on this with his keynote on the mineralogy of mudstones at Yellowknife Bay, Mars. Who knew that the best Earth-analog for these mudstones is also the entrance to the Bat Cave!
Today’s session on Coastal Archives of Climate Change was one of my highlights so far. Very interesting catching up with what has been happening in sclerochronology and related fields. Howard Spero showed some beautiful seasonal isotope records of oyster shells from Jamestown, Virginia, the first permanent English settlement in the Americas. Heather Black also spoke about oysters, but showed human influence in historic nitrogen isotope records.
Goldschmidt is also the conference where there are always lots of people that look at biomineralisation in great detail. This afternoon’s keynote by Susan Stipp was an excellent and engaging presentation on why this is relevant, and how some of the regulation on mineralization by organisms works.
For my own session and presentation I still have to wait until Thursday evening (posters) and Friday morning (orals). In the meantime there will be a lot more exciting science to hear about. You can follow some of it on Twitter #goldschmidt2014.
The poster I am presenting today at EGU2014.
For many of us being an early bird becomes progressively more difficult as conference fatigue takes its toll. I was glad to see a sizeable crowd managed to be there for the start of our session on the role of biominerals in biogeochemical cycling, which happened to be about birds and worms, and some other creatures.
Thomas Tütken showed us that the fearsome Eocene terror bird was neither a predator, nor a worm-catcher, but a gentle herbivorous giant instead! Also, the oxygen isotope composition of the bones of large herbivores forms a remarkably good archive of Cenozoic climate, agreeing well with the famous Zachos curve.
Then it was my turn to talk about worms, who are unexpected biomineralisers, and appear to precipitate atmospheric carbon dioxide in carbonate granules in the soil. Loredana Brinza studied metals in these granules, and demonstrated that they can significantly contribute to zinc immobilisation in polluted soils.
From animals we switched to plants, with two presentations about phytoliths: little chunks of silica produced by plants. Jean-Dominique Meunier and Eric Struyf showed that the contribution of phytoliths to global silicium cycling is much larger than previously thought and is of the same order of magnitude as the marine contribution of diatoms. Humans remove a lot of silicium from the global cycle by harvesting crops, and this likely reduces crop yields.
Going from the terrestrial to the marine realm, Ruth Carmichael spoke about nitrogen in bivalves and their potential for nitrogen sequestration as well as reconstruction of nitrogen cycling before human influences, using shells from middens that are thousands of years old. Adilah Ponnurangam stayed with the bivalves, but looked at rare-earth elements and showed that they reflect seawater composition.
The session ended with Michaël Hermoso presenting some meticulous laboratory culture experiments on coccolithophores, and size-related differences in carbon-isotope fractionation. All-in-all a very interesting morning, and a satisfying debut as a session chair.
Copper and iron isotopes vary with AB0 blood types.
I like it when people show how a proxy works, or how it doesn’t. Today at Goldschmidt I enjoyed several presentations doing exactly that. The day started with Johanna Noireaux showing that boron isotopes can only function as a pH proxy in aragonite, and not in calcite.
Anders Meibom presented work by Nehrke et al. demonstrating that contrary to what is commonly thought, foraminifera do not form most of their shell calcite from seawater that is ingested in vacuoles, but by active transport of calcium across the cell membrane. Vacuolisation does explain the presence of magnesium in foraminifera calcite, and also that the amount of magnesium is different between species, and depends on temperature (hence it’s such a good proxy).
Something else I’ve been keen to learn more about, is specific compound stable isotope applications. Yoshito Chikaraishi gave a very clear presentation showing that when bulk carbon and nitrogen isotope compositions look kind of messy, the compositions of specific amino acids can actually give us an accurate picture of the structure of a food web.
Geochemists’ second love (after geochemistry of course), must be food & drink. Apart from learning about trophic positions of various organisms, importantly we learned that a lot of the animals studied make excellent sashimi. When this afternoon I heard a speaker explaining the location of their sampling site mostly in relation to a BBQ restaurant, I knew it was almost time for beer and snacks, and posters.