The new edition of the Cypris IRGO newletter has now been published, and can be found on the ostracod group page of the website.
The new edition of the Cypris IRGO newletter has now been published, and can be found on the ostracod group page of the website.
Our first Special Issue of the Newsletter, with the abstracts from the 2021 annual meeting is now available to download.
The Micropalaeontological Society is delighted to announce the winner of the 2018 Micropalaeontology Image Competition!
The overall image winner was submitted by Robert P. Speijer from the Department of Earth and Environmental Sciences, KU Leuven, Belgium, with his beautiful image of the foraminifera Nummulites involutus Schaub, from the Ypresian clays near Kortrijk, Belgium. The image is a sperfect equatorial thin-section through a small (~ 3 mm) excellently preserved nummulite, and was scanned with a GE-Phoenix Micro-CT and the image was modified in Picasa. Not only does Robert win the competition’s first prize of €200, but also has his image included on the front cover of our TMSoc2019 Calendar (see above)!
On behalf of the Society we would like to congratulate Robert on his success. Eleven additional winners were selected from the fantastic submissions, and are on display below! A wide variety of microfossils and imaging techniques have been championed this year, and we are already looking forward to next year’s competition.
The twelve winning images have been incorporated into the 2019 Micropalaeontology Calendar, which will soon be available for purchase! Like last year, the calendar has been produced in spiral-bound A4 landscape format with one page per month.
A full list of the winners can be found below:
Robert P. Speijer, KU Leuven, Belgium (overall winner) – An equatorial section through for foraminifera Nummulites involutus Schaub. This is a small (~ 3 mm) excellently preserved nummulite from the Ypresian clays near Kortrijk, Belgium.
Please note, calendars are due to be ready for delivery by 10th November, so please be patient if purchasing calendars before this date
The meeting was organised and hosted by Alan Lord and chaired by John Whittaker in the Arthur Holmes Room of the Geological Society of London, Burlington House, Piccadilly.
John Whittaker gave a short update on the latest TMS Special Publications available via the Geological Society Publishing House. Initial reviews of “Ostracods in British Stratigraphy” have praised its presentation and quality of its plates, thoroughly recommending its purchase. John also described the official launch of the “Curry Volume” in Chichester on October 2nd attended by Dennis’ family.
Giles Miller (Natural History Museum) started off proceedings by showing us a series of beautiful 3-D plastic models (c.15cm long) of Pattersoncypris micropapillosa Bate 1972, created from the 3-D computer scans taken at the ESRF synchrotron at Grenoble. Apparently the models are created using two lasers focussed in to a bath of liquid resin that hardens where the beams cross. Ray Bate, who is donating them to the NHM, kindly paid for the models. Other models of such scans now form a display at the NHM based on recent research published in Science suggesting that ostracods were reproducing using giant sperm as far back as the Cretaceous (see TMS Newsletter No. 80, p.19 and search for ostracod on www.esrf.eu).
The field trip comprised a tour of Silurian age localities in the Malvern Hills area (now part of the Abberley and Malvern Hills Geopark). The group met at British Camp Hillfort on the morning of the 17th and proceeded to Gullet Quarry, well known for its Llandovery conodonts.
Once we had arrived at the quarry, a bottle of champagne was opened to celebrate Dick Aldridge’s “significant” birthday, the quarry being one of the localities from both his undergraduate mapping and his PhD. After a while talking and catching up we were then met by Dr Peter Oliver, director of the Hereford and Worcester Earth Heritage Trust who welcomed us to the geopark and gave a brief talk about the geology of the area.
Queen Elizabeth II Conference Centre, London, 6th – 9th October 2003
Previously this conference has been held at the Barbican Centre, leading to the conference being widely known as the Barbican Conference. This year the Queen Elizabeth II Conference Centre was used as the new venue, enabling both a core workshop and a 3D visions session to run alongside poster presentations and up to 4 parallel talk sessions. I think everyone would agree that the setting for the conference was unsurpassable, even for those working in London, with Big Ben, Westminster Abbey and the Houses of Parliament on the doorstep.
The conference, though still mainly concentrating on exploration and development in north-western Europe, did this time include presentations of global interest. And although initial registration numbers showed a slight decrease in numbers since the last time the conference was held, by the time the late entrants had registered, the number of delegates was on par with previous years.
Extant coccolithophores have attracted a wide range of research over the past decade including much research on topics such as dimethyl sulphide and alkenone production, physiological ecology, carbon uptake mechanisms, remote sensing and modelling of blooms, but also taxonomy-based research on biodiversity, molecular genetics, ecology, biogeography and flux estimation. As a result of the latter strand of research there is now a significant number of specialists world-wide who are identifying and studying extant coccolithophores.
Reston, Virginia, U.S.A. 21st.-23rd. September 2003
In late September, and immediately after the landfall of Hurricane Isobel, the U.S. Geological Survey hosted an ICDP (International Continental Drilling Program) workshop at Reston, Virginia to define the scientific criteria which will decide the location for a deep well to be drilled in the centre of the Chesapeake Bay Impact Crater (CBIC).
The CBIC impact occurred approximately 35 million years ago (Late Eocene) when a meteorite or comet came to earth on the U.S. Atlantic continental shelf at a location that is currently occupied by the southern part of the Chesapeake Bay and neighbouring land, within the Virginia Coastal Plain. The crater as currently defined is approximately 84 km (53 miles) circular structure. This lies under several hundred feet of younger Tertiary marine sediments. Read more