blue-crab

User login

Powered by Drupal, an open source content management system
Follow Me on Pinterest

Care to comment? See our FaceBook page

The Bubbling Reefs

Imagine a beautiful shallow green water reef with kelp, anemones and sponges among which lots of colourful fauna darting in and out and. Now imagine that the reef is growing on some weird sandstone arches and that the water is fizzy like sparkly mineral water, with bubbles coming out of the reef structure.
The Bubbling Reefs
Published in X-Ray Issue: 23 - May 2008
Authored by: Peter Symes | Photography: | Translation:
Download pdf â–ş The Bubbling Reefs
At first glance, from a distance, the shallow stone reefs in the shallow water off the northern peninsula of Jutland, Denmark, does not seem to be much out of the ordinary. Diving in Denmark is all right—it has it moments and decent locations, but cannot compare to the often exceptional diving that the other brethren Scandinavian countries can offer—with a few exceptions, and this is one of them.
share

As you get closer, you will soon realise that this location is anything but ordinary. The thriving reef is not only full of interesting macro life—in large part thanks to the marine reserve status the area enjoys—but delicate arches and pole-like structures poke out of the sand. The overgrowth of kelp and sponges gives them a furry appearance. But it is the slow fizz of bubbles coming out from the inside of these structures that gives the dive experience here a definitely surreal tint.

So, what’s going on here?
The gas is methane, and what lies beneath the seabed is what you could call an oil field still in the process of forming.

The methane most likely stems from microbial decomposition of plant material deposited during the Eemian and early Weichselian periods, i.e. 100,000 to 125,000 years B.P. The gas then seeps up through the sandy seabed forming channels, or funnels, along the paths of least resistance.

As other aerobic microbes in the upper layers oxidise the methane, they turn the loose sand into solid carbonate cemented sandstone structures. It is believed that the cementation occurred in the subsurface, and that the rocks were exposed in the open by subsequent erosion of the surrounding unconsolidated sediment. In other words, the surrounding sand was later washed away by changing currents, leaving the solidified parts standing free as a sculpture garden.

These structures can be up to 500 m2 and consist of columns up to four meters high, arches, complex formations of overlying slab-type layers, and pillars up to 4m high. The rocks support a diverse ecosystem ranging from bacteria to macroalgae and anthozoans.
Many animals live within the rocks in holes bored by sponges, polychaetes and bivalves. Within the sediments surrounding the seeps, the abundance and diversity of metazoan fauna

Download the article to read the full story â–ş The Bubbling Reefs
Advertisements