2025 BCRA Online Seminars via Zoom
Our monthly seminars are intended to promote the scientific importance of caves and karst,
and they describe ways in which BCRA supports cave research. Some of these talks are jointly
organised by BCRA and the Ghar Parau
Foundation. GPF is a charity that provides grants to British caving expeditions throughout
the world. These talks will use the Zoom platform.
If, as part of this series of seminars, you would like to offer a talk on a science
topic that you think would be of interest to a broad caver audience then please
contact John Gunn with a title and a few words about your suggested
content.
Click/Tap a link or scroll on down.
Past
Seminars in 2025
Click the pull-down icon to show/hide the list.
#1 — Mon 13 Jan 2025 ▼
Microbial Nitrogen Cycling and Cave Passage Modification in Mulu National Park
With: J. Max Koether, Department of Geology, University of Alabama
Time: Mon 13-Jan 2025, 19:30 to 21:00 GMT.
To Watch: see Joining via Zoom.

Photo: J. Max Koether
Research into how caves form increasingly reveals the critical role of microbes in promoting chemical erosion through
the production of acidic byproducts. The caves of Gunung Mulu National Park in Sarawak, Malaysia, offer a setting to
explore a novel nitrogen-driven method of cave passage modification and enlargement. These caves include some of the
world's largest and longest cave systems, including Clearwater Cave, which extends over 250 kilometers, and many of
these caves feature unusual formations, such as massive ceiling scallops and corroded speleothems. We suggest that these
distinctive features result from dissolution caused by microbial activity.
Microbial activity within the nitrogen-rich guano from birds and bats in the caves generates ammonia gas. This ammonia
adheres to moisture on cave walls, where microbes recapture the ammonia and metabolize it, producing nitric acid as a
byproduct and leading to the chemical dissolution of the rock. Using several analytical techniques, both in the field
and in the lab, we propose that nitrogen-driven dissolution is a common process in tropical caves, and that this
mechanism may play a significant role in enlarging cave passages after their initial formation.
#2 — Mon 10 Feb 2025 ▲
Sulfuric Acid Speleogenesis: how can we recognize it and what can it teach us?
With: Jo De Waele, Professor, Dept. of Biological, Geological, and Environmental Sci., University of Bologna
Time: Mon 10-Feb 2025, 19:30 to 21:00 GMT.
To Watch: see Joining via Zoom.

Photo: Orlando Lacarbonara
Although sulphuric acid caves (SAS Caves) have been known of for over two centuries (Socquet described a SAS cave in
Aix-les-Bains in 1801), these caves were considered as "geological oddities". They rank among the "hypogene" caves, and
are important for the understanding of void formation not directly connected to present-day meteorology and surface
morphology (e.g., hydrocarbon reservoirs, Mississippi valley type Pb-Zn ore deposits). Since the discovery of
Lechuguilla Cave in New Mexico and Movile Cave in Romania (both in 1986) speleological and karstological research has
intensified and many more SAS caves have been discovered and recognized.
Today over 90 SAS cave occurrences have been reported around the world, and their number is increasing steadily as
cavers have started to recognize their typical morphologies and by-products. This talk, prepared in collaboration with
Ilenia Maria D'Angeli, will show the distribution of SAS caves in the world, the different typologies, their unique
morphology and by-products, their role in understanding landscape evolution, and their intriguing microbiology and
biology.
Our Seminar Programme
#3 — Mon 10 Mar 2025 ▼
The Underground Mistakes of My Career. Lessons Learned from Maaras Cave, Greece.
With: Christos Pennos, Aristotle University of Thessaloniki, School of Geology, Thessaloniki, Greece.
Time: Mon 10-Mar 2025, 19:30 to 21:00 GMT.
To Watch: see Joining via Zoom.

Photo: Christos Pennos
In this talk, I will present data collected from Maaras Cave over the past seven years, focusing primarily on
hydrogeology and geomorphology. The Maaras Cave system is located along the northwestern margin of the Aggitis River
basin. It contains an active fluvial system fed by a closed karstic basin, the Kato Nevrokopi polje, to the northwest.
The cave is formed within the marbles of the Rhodope Massif and exhibits a distinct morphological pattern. It lacks
closed loops and follows a hierarchical structure, where lower-order tributaries merge into higher-order passages. The
system consists of two main tributaries, an eastern and a western branch—that converge into a single conduit flowing
toward the spring a typical branchwork cave following Palmer's classification.
#4 — Mon 14 Apr 2025 ▲ ▼
Palaeontological Perspectives on Caving in Thailand
With: Spyridoula Pappa, Senior Curator of Fossil Mammals, Natural History Museum
Time: Mon 14-Apr 2025, 19:30 to 21:00 BST.
To Watch: see Joining via Zoom.
This is the talk postponed from December 2024

Photo: Spyridoula Pappa
If you want to know more about caves and fossil mammal remains from Mae Hong Son Province, in north-western Thailand,
then join me for this talk where I am going to share everything from my most recent research fieldwork in Thailand, in
January 2024.
One of the most interesting and important sites that I visited was Tham Lod rock shelter where I sampled teeth fron
Eld's deer. Tham Lod is a magnificent and famous cave and a well-stratified archaeological site, where more than 100,000
archaeological items were unearthed during previous excavations. I and my NERC DTP PhD student Laura Hemmingham have had
the opportunity to collect samples of over 200 fossil deer teeth, excavated from several Thailand caves and open sites.
Through the Eld's deer project we studied the diet of Pleistocene deer in relation to climate using the methods of
dental wear analysis (DWA), mesowear and species distribution models. My research focuses on palaeoecology of the
Quaternary and I am analysing tooth material to understand what these animals ate during the Ice Age and how they
responded to environmental and ecological changes.
I started caving in 2002 and have participated in multiple caving expeditions with the Hellenic Speleological Society
and with speleologists from Vienna University. I completed my undergraduate degree in Geology, and my Masters degree in
Palaeontology, in Greece. My PhD in Palaeontology was from Royal Holloway University of London. I moved to London in
2010 and since September 2015 I have been working as a curator in the Natural History Museum (NHMUK). I am responsible
for fossil mammals (over 350,000 specimens from around the world). During this talk I will be also presenting tales and
projects that I had the opportunity to work on from other European and UK cave sites.
#5 — Mon 12 May 2025 ▲
Limestone, dirt and iron: using cave magnets to understand the past
With: Bethany Fox, Senior Lecturer, Dept. Biological and Geographical Sciences, Univ. of Huddersfield
Time: Mon 12-May 2025, 19:30 to 21:00 BST.
To Watch: see Joining via Zoom.
Contact email: B.Fox@...

Photo: Bethany Fox
The natural world is full of tiny magnets: in the soil, in the water, and even in caves. These magnets have fascinating
histories that can tell us about changes in the Earth's magnetic field, about rainfall and temperature, about soil
microbes and even about industrial pollution. While scientists have been studying natural magnets for many years, it is
only recently that magnetometers have become sensitive enough to measure the magnetism of cave deposits, like
stalagmites and stalactites. This talk will introduce the wonderful world of cave magnetism, focusing particularly on
our recent magnetic study of the flooding history of Waipuna Cave, New Zealand.
Joining via Zoom
You are advised to download and install the Zoom program in advance, from
Zoom Client for Meetings
. If you do
not do this in advance you will be prompted to do it when you join a meeting, and you could have
to spend a few minutes installing it and working out how to use it. It is also possible to attend
a Zoom meeting via a web browser, but this is not recommended unless you cannot get Zoom to
install properly.
Join the next BCRA Zoom Meeting
You can test your connection
prior to
the meeting
- If you try to join the meeting before the host enables it, you could be left "in
limbo". Therefore, if your computer has not connected by, say, five minutes before the scheduled
start time, please log out and log back in again.
- If you cannot log in at all, please check our
Facebook page where
we will post any last-minute messages concerning, for example, any technical problems that we are
having.
- We might be using a Zoom passcode for this meeting. If so, it will be displayed
in a pop-up alert when you click on the link. You will need to note it down and enter it manually
when you are taken to the Zoom login page. Some devices might not be able to receive pop-up
alerts. Click here to
test whether you can receive these alerts. If you cannot then you will need to contact us, in
advance of the meeting.
- Please note that this event will not be recorded by BCRA. You can only watch it live,
via Zoom. The reasons for not recording our seminars are because a) obtaining the necessary
copyright clearances can be difficult, and time-consuming; and b) some content may be subject to
embargoes or other academic constraints. If you are interested in obtaining the content of a
particular talk you should contact the speaker privately.
Seminars Archive
View talks given in 2021, 2022 (none), 2023, 2024, 2025.
Notes for Staff
Notes for IT
- Slide timings are set in the JS variable $global_slide_times in
slides.js.
- The index number of the image to use for the Facebook scrape is set in the JS variable
$talk_for_OGI in seminar_data.js
- After Facebook has been allowed to scrape an image URL, if that image needs to be
changed, then it must be given a new URL in seminar_data.js. Thus if, initially,
$data["use_image"][7] = "/img_lib/talks23-7.jpg" then that must be updated by, say, adding
a version number (e.g. 23A-7) or Facebook will not attempt to re-fetch the file. If the
above syntax is preserved, the new "use_image" filename will still map to the correct actual file
name, as set in $data["image"] .
- When running at localhost a debug dump follows. (HTTP_HOST = bcra.org.uk).
get_included_files() is