"Cave biofilms are simpler than the microbes that occur in soils where there can be hundreds of thousands of species," says Dr. Jennifer L. Macalady, assistant professor of geosciences, Penn State. "Some cave biofilms have very few species, 10 to 20. The more complex ones have 100s or 1,000s."
The researchers investigated the Frasassi cave system located north of Rome and south of Venice in Italy. These limestone caves are like New Mexico's Carlsbad Caverns and Lechuguilla
Cave, but in those caves, sulfur entered the caves from oil and gas reserves, while in Italy, the sulfur source is a thick gypsum layer below. Having sulfur in the environment allows these biofilms to grow.
Most limestone caves form when rainwater and runoff permeate the caves from above. Water and carbon dioxide mix to form carbonic acid, a very weak acid, that erodes the limestone cave walls. In sulfidic caves, water enters the caves from below, carrying hydrogen sulfide. Microbes in the biofilms use the sulfur for energy and produce sulfuric acid, a very strong acid.
"One type of biofilm, called a snottite because of its appearance, has a pH of zero or one," says Daniel S. Jones, graduate student in geosciences. "This is very, very acidic."
Carbonic acid cave systems lose about a third of an inch of wall every thousand years, while sulfuric acid cave systems lose about two and a third inches or six times as much in the same time. The researchers are interested in the make-up of the biofilms and how they cycle sulfur.
Biofilms are made up of thin layers of microbe species that can be very different. All require water, but some biofilms live in the pools, lakes and streams in caves and others live on the damp walls. The layers against the rock surface use oxygen and hydrogen sulfide for energy and produce sulfuric acid. The layer on the outside does as well, but, because middle layers exist, there is an opportunity for microbes that find oxygen poisonous to thrive. These middle layers may convert the sulfuric acid to hydrogen sulfide, creating a complete sulfur cycle in a few microns.
In dental biofilms, the microbes on the teeth are the ones that produce the acids that cause cavities, while the ones on the top create the right conditions for the acid-producing microbes to survive. Cave biofilm layers also fulfill different niches in their very tiny environment.
"Stream biofilms are responsible for the majority of sulfide disappearance in streams," Jones told attendees today (Dec. 11) at the fall meeting of the American Geophysical Meeting in San Francisco.
Because the cave biofilms are relatively simple, it will be easier to connect the various microbe species to the geochemistry involved. While this work is not yet complete, the researchers are working on the problem. Dr. Greg K. Druschel, assistant professor of geology, University of Vermont, used microelectrode voltammetry to try to determine exactly which biofilm layers produce acids. The levels of hydrogen sulfide and sulfuric acid change, depending on which layer is tested.
"There is also a question about where these microbes originate," says Macalady. "We do not know if they are always in rocks or if they are transported from somewhere else to establish themselves."
No matter the answer, the biofilms probably begin growing in tiny cracks in the rock and eventually create some of the largest cave systems in the world. Cave biofilms are also the bottom of the food chain for cave ecosystems. They provide food for a variety of spiders, flat worms, pill bugs and amphipods – shrimp like crustaceans – that form a blind and pigmentless community.
"The only other place we find sulfur-based ecosystems is near the deep sea vents on the ocean floor," says Jones.
Understanding how cave biofilms dissolve calcium carbonate may help us to understand the communities around ocean floor vents, but it may also, eventually, lead to understanding how biofilms dissolve calcium phosphate on teeth and the steel hulls of ships.
A 3-D look at the 2015 El Niño
29.05.2017 | NASA/Goddard Space Flight Center
'Tiny clocks' crystallize understanding of meteorite crashes
29.05.2017 | University of Western Ontario
The world's highest gain high power laser amplifier - by many orders of magnitude - has been developed in research led at the University of Strathclyde.
The researchers demonstrated the feasibility of using plasma to amplify short laser pulses of picojoule-level energy up to 100 millijoules, which is a 'gain'...
Staphylococcus aureus is a feared pathogen (MRSA, multi-resistant S. aureus) due to frequent resistances against many antibiotics, especially in hospital infections. Researchers at the Paul-Ehrlich-Institut have identified immunological processes that prevent a successful immune response directed against the pathogenic agent. The delivery of bacterial proteins with RNA adjuvant or messenger RNA (mRNA) into immune cells allows the re-direction of the immune response towards an active defense against S. aureus. This could be of significant importance for the development of an effective vaccine. PLOS Pathogens has published these research results online on 25 May 2017.
Staphylococcus aureus (S. aureus) is a bacterium that colonizes by far more than half of the skin and the mucosa of adults, usually without causing infections....
Physicists from the University of Würzburg are capable of generating identical looking single light particles at the push of a button. Two new studies now demonstrate the potential this method holds.
The quantum computer has fuelled the imagination of scientists for decades: It is based on fundamentally different phenomena than a conventional computer....
An international team of physicists has monitored the scattering behaviour of electrons in a non-conducting material in real-time. Their insights could be beneficial for radiotherapy.
We can refer to electrons in non-conducting materials as ‘sluggish’. Typically, they remain fixed in a location, deep inside an atomic composite. It is hence...
Two-dimensional magnetic structures are regarded as a promising material for new types of data storage, since the magnetic properties of individual molecular building blocks can be investigated and modified. For the first time, researchers have now produced a wafer-thin ferrimagnet, in which molecules with different magnetic centers arrange themselves on a gold surface to form a checkerboard pattern. Scientists at the Swiss Nanoscience Institute at the University of Basel and the Paul Scherrer Institute published their findings in the journal Nature Communications.
Ferrimagnets are composed of two centers which are magnetized at different strengths and point in opposing directions. Two-dimensional, quasi-flat ferrimagnets...
24.05.2017 | Event News
23.05.2017 | Event News
22.05.2017 | Event News
29.05.2017 | Physics and Astronomy
29.05.2017 | Physics and Astronomy
29.05.2017 | Earth Sciences