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ure News 11 - Gibraltar Ornithological & Natural History Society

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1ST INTERNATIONAL CAVE MONITORING FIELD WORKSHOP<br />

Jointly organised by Royal Holloway, University of London, University of Innsbruk<br />

and the <strong>Gibraltar</strong> <strong>Ornithological</strong> and <strong>Natural</strong> <strong>History</strong> <strong>Society</strong>.<br />

Monitoring headquarters, St Michael’s Cave<br />

In February, GONHS will be hosting the worlds<br />

first International Cave Monitoring Field Workshop.<br />

This will be a four-day event bringing cave and climate<br />

science specialists from all over the world to<br />

<strong>Gibraltar</strong>. Climate change studies have been a hot<br />

topic now for quite a few years involving different<br />

approaches to understand what the climate was like<br />

in the past. <strong>Gibraltar</strong> is in a uniquely important location<br />

to carry out this research not only because of its<br />

geographical location at the junction between two<br />

continents and two oceans but also because of the<br />

abundance of caves containing stalagmite records of<br />

past climates and long history of weather recording<br />

since the 18th century.<br />

Scientists involved in climate studies use a range<br />

of different specialised fields to uncover the past. For<br />

example, botanists can use tree rings to get a climate<br />

record over the last few millennia, scientists in polar<br />

regions take very long ice core samples spanning tens<br />

of thousands of years which provide a record of the<br />

atmosphere when the snow and ice were formed.<br />

Exactly the same happens when a stalagmite in a<br />

cave grows. The “rings” in a stalagmite corresponds<br />

to a layer of growth in the life time of the speleothem<br />

and may record the rainfall over periods spanning<br />

many seasons to individual storms. Stalagmites, like<br />

ice cores, tree rings, mud cores and even human hair,<br />

record a detailed record of what the environment was<br />

like when they grow undisturbed, sometimes over<br />

hundreds of thousands of years. The problem with<br />

most ‘proxy’ climate records such as pollen, tree rings<br />

etc. is that while they reveal general trends in climate<br />

(warmer-cooler, wetter-drier etc) they do not provide<br />

hard data (temperat<strong>ure</strong>s, rainfall amounts, weather<br />

patterns) that the climate modellers (the scientists that<br />

provide the all important predictions of the fut<strong>ure</strong><br />

weather) badly need. Stalagmites are one of the only<br />

proxies that have the potential to do this but only if it<br />

is known how the cave temperat<strong>ure</strong> and groundwater<br />

responds to different weather patterns.<br />

In 2004 The Royal Holloway University of<br />

London in partnership with the GONHS initiated an<br />

innovative research program on how a caves really<br />

work and how accurately stalagmites record the past<br />

climate. The study, supported by the UK <strong>Natural</strong><br />

Environment Research Council, initially focussed on a<br />

small sample of a stalagmite from New St Michaels<br />

cave was taken to the hi-tech research laboratories in<br />

the Earth Sciences Department at Royal Holloway.<br />

Using laser systems and computer controlled<br />

micromilling instruments the isotopic record of the<br />

sample was investigated at the highest resolution ever<br />

made and provided the first ever record of monthly<br />

variations in growth of an active speleothem which<br />

could be accurately related to the weather above the<br />

cave.<br />

At the same time data logging systems were<br />

deployed in and around the cave, and in the soil horizons<br />

above the cave, to record temperat<strong>ure</strong>s, humidity,<br />

groundwater flow and air compositions. These<br />

systems have been managed by<br />

the Caves and Cliffs section of<br />

GOHNS who also carried out regular<br />

monthly sampling of groundwater<br />

and air for further analysis.<br />

Some of the gadgets needed, such<br />

as drip counters, carbon dioxide<br />

sensors and loggers were specially<br />

designed for this project and have<br />

provided data that have never<br />

been obtained for a cave system<br />

anywhere else in the world. Along<br />

with cave monitoring, the project<br />

has accrued numerous other firsts,<br />

ranging from using the latest techniques<br />

for analysing and imaging<br />

stalagmites at the European<br />

Synchrotron Facility in Grenoble,<br />

and resurveying the St Michaels<br />

system by precision laser scanning<br />

which is producing a highly accurate<br />

3-D computer model of the<br />

caves.<br />

After four years of hard work<br />

we have been able to show that<br />

cave monitoring is essential in<br />

order to understand the links<br />

between weather events and how<br />

these are recorded in stalagmites.<br />

The results of this research have<br />

provided some very interesting and<br />

sometimes unexpected results. We<br />

have found that cave ventilation is<br />

one of the most important controls<br />

on stalagmite growth and New St<br />

Michaels cave, takes two breaths a<br />

Kevin Dixon using a laser scanner<br />

to image the Lake Chamber<br />

year: it inhales in winter and exhales in summer. This<br />

has huge significance to the way stalagmites record<br />

climate and was only discovered whilst doing the<br />

study. Another important part of the project is understanding<br />

the passage of water as rain into the cave.<br />

The calcite that forms into a beautiful stalagmite is<br />

brought in by rainwater that has picked up carbonic<br />

acid as it travels through soil and dissolves rock along<br />

bedding planes, and deposits the calcite on the stalagmite<br />

has a new layer. Knowing exactly how long it<br />

took that rain water to appear in the cave is therefore<br />

important. For example, in an area of the cave we<br />

have sites just a few meters apart that respond completely<br />

differently – one has a response time to rain of<br />

only 6 hours others responds far more slowly. At<br />

another site water is now known to pass though a<br />

siphon type reservoir, indicating that the water is<br />

being stored before reaching the cave. All of these<br />

different responses meas<strong>ure</strong>d across 4 years of monitoring<br />

have important effects on the way the<br />

speleothem grows and records climate.<br />

<strong>Gibraltar</strong> is now at the forefront of this field of<br />

research and in February we will be welcoming the<br />

cave science community from the US, Australia and<br />

all over Europe to discuss monitoring techniques and<br />

interpretation of climate records in cave deposits. A<br />

highlight of the meeting will be underground visits to<br />

see the cave monitoring systems running and gathering<br />

data which have now achieved international<br />

recognition.<br />

References<br />

Mattey, D., Latin, J.-P. and Ainsworth, M. Cave<br />

monitoring and calibration of a δ18O – climate<br />

transfer function in <strong>Gibraltar</strong>, PAGES <strong>News</strong>letter,<br />

16(3): 15-17, 2008<br />

GIBRALTAR NATURE NEWS<br />

<strong>11</strong>

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