Cryptobiotic Soils and Lichens of Joshua Tree National Park - Date Book

Cryptobiotic Soils and Lichens of Joshua Tree National Park - Date Book

Link to a short field course at Joshua Tree National Park taught by Nicole Pietrasiak and Kerry Knudsen.

The web presence of the biocrust research community: a request for participation and ideas

It seems to me that right now, we are seeing an unprecedented interest in the science of biological soil crusts. There are more and more of us in more places conducting this research. Nevertheless, our field is still young and at this moment all of us are more like allies than competitors. We do what we do because we think it is important, fascinating and under appreciated and for the most part we are happy to see another succeed in the same area. In my opinion, we should channel this energy to coordinate our web presence as a research community. I think this can only benefit us as our science becomes "mainstream". I argue below for the value of blogging, online forums, researcher directories, and dynamic bibliographies.

Why not just build a really good static website like soil crust.org? Well, first, there already are more than one static site that are good. In addition to these good existing sites, we also need a dynamic platform with content that changes daily, and a mechanism for two-way talking (comment boxes). So we are talking about something dynamic and interactive. We are in a rapidly growing field and stuff changes all the time. I think of  a good static website and a good dynamic website as complementary, especially if they are cross-linked in a prominent location (for example, here I link soil crust.org on my top bar), which recognizes it as a sister site. What do others think?

So what web resources do we need?

1. A platform for non-technical dissemination of our work. I think that blogs are here to stay for a while and are a logical medium for this. Scientists has a very serious communication problem with people that aren't also scientists. Science blogging is emerging as a real, impactful medium to communicate science. It doesn't replace technical publications in journals, but complements it very well. Many journals now have excellent blogs written by the editors. There are aggregators which collect and repost blog entries about scientific research. This blog you are reading gets about 50-100 page views per day. Now, that is not exactly viral. BUT, that rate of viewing absolutely shatters the rate of traffic my actual papers get. This is an emerging element of scientific impact that we should take part in. Usually governments fund our research with revenue derived from taxes. People that pay the taxes deserve to be able to read about the science that gets funded if they wish to.

Let me illustrate the significance of communicating with non-scientists. Recently Alan Savory did a TED talk promoting his high-intensity rotational grazing method as a way to reverse desertification and climate change. His talk was simple, compelling, and easy to understand. Alot of intelligent people asked me what I thought about this "great" talk. The truth is it was unsubstantiated by data and evidence, plagued by logical flaws, completely wrong in my opinion, and maybe dangerous. He actually refers to "algal crusts" as a symptom of a cancer of the land. He got over 1 million hits, and miseducated about that number of people in my opinion.

How can we counter that? We probably can't now in that particular case, unless we get Jayne to do a TED talk, but it speaks to a need for us to create and disseminate freely available and understandable interpretation of good science and data on a regular basis. We can't complain that people are only picking up bad information if we don't put out good information that a non-professional can read.

The other nice thing about a base blog platform is that comments can be left on posts for anyone to read. This is a good space for researchers to discuss the topic of whatever a given post is about. Also it's a way to interact with members of the general public with an interest in biocrust science.

2. A networking resource. I suggest that a group forum that is viewable to the general public is the best platform for us to communicate freely with each other (see above and below). I currently have one embedded in this blog. Its new. Follow the link "Geodermatophilia Forum" above in the top bar or here. Anyone can select a topic of their choice, and leave a comment. You do not have to have a special account or anything. You will recall list-serves and probably still use some. That is a 20 year old technology, a forum is better.

3. An online, comprehensive biocrust bibliography that can be updated. Scott Bates, Jayne Belnap, Nichole Barger & I have all talked about some form of this at various times. Different people have somewhat different visions, but we all recognize how useful this would be. There is a static one on soilcrust.org, but it needs an update and maybe a format change which Jayne spoke about at BIOCRUST 2013 in Madrid. 

Here's another related idea. Wouldn't it be great if not only were this a bibliography, but a massive shared, searchable collection of pdfs. Maybe Mendeley is the platform? How can we do this, what ideas do people have and how will we accomplish it? This is a great topic for discussion on the forum.

4. A biocrust researcher directory. Currently I have a shoddy version on the right sidebar of this blog. It is not comprehensive, it is just what I had time to piece together. I can envision a standalone page where each researcher has a little bio, contact information, maybe a picture, and a set of links to their other pages if available. Are there other ideas? Leave them on the forum.

5. I dont know. What else do we need, web-wise? Let's discuss it here.

Why a blog rather than, e.g., twitter, facebook? 
Twitter & facebook are great ways to quickly share small snippets of information with lots of people. A blog can do this too, but in addition, a blog is a more complete platform for collecting and listing links and short articles. Also, this blog contains simple buttons at the bottom of each post that allows you to share posts on twitter or facebook. The posts here automatically aggregate to two science blog aggregators, Scienceseeker.org & natureblognetwork.com. With a couple extra steps, posts about published papers can also be published on my personal favorite researchblogging.com. Take a minute and look at these sites, don't you agree that this is a great way to get information out on the web?


When I established the blog you are reading, I did not envision it as "my" blog, I envisioned it as our networking resource. The only way this can actually work is for people to participate and engage. 

Ways to participate in this website (listed from most active to passive):
1. Be a poster. Write on this blog. A post can be as simple as a tweet, e.g. sharing a link,  that costs seconds or an in-depth piece that might require hours. All you need to do is tell me that you want to post, and I will get you set up and you can post as little or as much as you want. Not only can this help disseminate information to the public, but it can help you direct readers to your own work and establish you as a voice to listen to on the topic of biocrusts. So, it's a fun way to spend free time (i.e. a hobby) that can also promote your career. I enjoy bicycling too, but that doesn't promote my science, so I think this is a good deal.

What should you post?

Here's some ideas to get started: a. Share your photos, b. Discuss a paper or news story, c. Update us on your lab activities, d. Cross-post from your other blogs or lab webpage, e. advertise for jobs, books, conferences either in the blog page or the forum, f. review equipment or sell used equipment, g. promote and summarize your recent research, h. post radio or video pieces that you run across relevant to arid lands, crusts, dust, j. find a collaborator or partner on a proposal, k. post a link to your archived data, etc., l. post course plans or curricula for class activities involving biocrusts. m. write a tribute post about a prominent biocrust researcher that is retiring.

2a. Leave comments on blog posts. Commenting on blog posts leads to public conversations and discussions that can be insightful.

2b. Leave messages on the forum. For example, you can: a. enlist help from the crust community (e.g. "Someone please tell me the best way to measure Chlorophyll a using a Synergy HT plate reader", "How can I distinguish Fulgensia species in the field?", etc.)j. b. find a collaborator or partner on a proposal, c. post a link to your archived data, etc.

3. Share things that ought to be posted or linked with a poster. The poster, with minimal effort can share it.

4a. If you are a biocrust researcher & you have some form of website, check to be sure you are in the researcher directory to the right. Make sure the best possible link is used, otherwise give me the information to change it.

4b. If you maintain a website, please consider linking this one. The more links, the higher the site in Google.

5. If you like a post, share it using Facebook, Twitter, Google + other social media. At the bottom of each post there are buttons that allow you to do so easily - just push and enter login details. Also simply tell people about the site.

6.  "Follow" the blog, using your google ID. When you log into google all new posts of the blogs you follow will come up. If you use a blog reader, any new posts will automatically be forwarded there (it's like friending someone in Facebook). Also it is a visible "vote" that you like the content of this webpage, this encourages other to do so also.

7. Bookmark the blog & visit often. Traffic follows traffic, the simplest and most passive way to promote a biocrust website is to visit and read it.

OK, that's my pitch and it is especially focused on younger researchers (grad students, post-docs, new professors and the like). 

In summary please: Tell me if you want to post on the blog (you can tell me via email, the forum, or the comment box below). Use the forum to communicate your ideas about our community web presence. 

New! Forum is up and running

Look up at the top banner on this page, there are now multiple pages, one of which is labeled "Geodermatophilia forum". Follow that link or this one to the forum. Bookmark it.

This is a place where anyone can leave a comment or announcement. This is a distinct tool from the comment boxes at the bottom of posts because any topic can be discussed at any time (not just the most current blog post, and because its more conducive for reader-to-reader communications rather than poster to reader communication. AND, it is organizable into threads or topics.

Examples (not at all exhaustive) of good usage of this forum:
1. Back & forth discussion of threads
2. Advertise positions in your lab
3. Seek or give advise about taxonomy, methods, equipment, etc
4. If you are a member of the general public, ask a general question of the experts.

It won't have any value unless people use it, so please use it. It might require a little extra effort at first.

Fall 2013 Biocrust symposium in Flagstaff, Arizona

There have been alot of events lately promoting biocrust science. Three years ago the first international biocrust conference was held in Germany. Two years ago, there was a biocrust symposium at the Biennial Conference for research on the Colorado Plateau. Last Spring there were two such sessions here and here at The European Geosciences Union in Vienna. Last Summer, there was a special session at the Ecological Society of America Meeting in Portland which resulted in a special issue in the journal Ecological Processes. And in less than a week the second international biocrust meeting will kick off in Madrid. I'd like to continue this drumbeat by contributing another Fall Symposium in Flagstaff, Arizona. My draft speaker list and the topics are below, when final I will post all the titles and abstracts here. Although I've only got 16 symposium spots, I'd like to encourage all regional biocrust enthusiasts and researchers to attend or submit a talk or poster to the general conference...the more the merrier.

The Biennial Conference for Research on the Colorado Plateau is coming up September 16 - 19 in Flagstaff, Arizona. Kyle Doherty and I are co-organizing a symposium on biological crusts, which will occur on Wednesday (17th).

This is a very fun regional conference well attended by university and agency scientists, and many land managers as well.

conference website - http://nau.edu/merriam-powell/biennial-conference/

I tend to believe that the Colorado Plateau is one of the crust capitols of the world, due to its highly visible and charismatic biocrusts, and due to the relatively large number of researchers studying this topic. This will be the third such session at this conference, the most recent being two years ago. Two years ago (read about it here http://geodermatophilia.blogspot.com/2011/10/its-finally-on-colorado-plateau.html and here
http://biocrust.posterous.com/ we had a great lineup of talks on all topics biocrusty, with crust researchers in attendance representing Arizona, Utah, California, Colorado, Colombia, China and Catalunya. The session was packed, especially early, and well-attended by agency personnel who are keen to learn about biocrusts. In the late afternoon, we had our own private poster session, and a lovely night out featuring good beer, wine and bluegrass. It was great fun, and we'd like to continue the tradition. In addition to this biocrust session, Jayne Belnap will also be organizing a session on dust which will be of interest to many (myself included).

Biennial Conference for Research on the Colorado Plateau, Flagstaff, AZ, September 16-19 2013

Proposal for Symposium

Length: 4 hours

Title: Biological Soil Crusts: Response to climate change and utility in ecological restoration

Justification: Biological soil crusts (biocrusts) are the protective skin of the earth creating soil stability, building and maintaining soil fertility and influencing hydrology. Ecosystem functions of biocrusts operate from microscopic to landscape scales. They are one of the most informative indicators of terrestrial ecosystem health in the Colorado Plateau region. We wish to continue an incipient tradition of biocrust-themed sessions at the Biennial conference.

This special session is designed to bring together researchers from multiple western states working on two focal aspects of biocrust research. The session will focus on: 1. Responses of biocrusts to climate change and ecosystem consequences, and 2. Ecological restoration of biocrusts, theory and technology, 3. Biocrust genomics, metabolomics and microbial ecology. Speakers will be asked to tailor their talks to both a scientific and natural resource management audience. This session will complement a distinct session on the dust cycle the following day.

Expected outcomes: This session will give regional biocrust researchers the opportunity to disseminate their research and its relevance to resource management professionals. We will outreach also to alternative energy and military representative, two groups which may have special interest in biocrust restoration technologies. Equally important, especially for early career researchers, is the opportunity to network and meet peers. Multiple graduate students, post-docs and other early career researchers have been invited to participate. Symposia such as these lead to friendships, collaborations, research proposals, and more research conducted on these integral components of Colorado Plateau ecology.

Available funding: None has been secured. Speakers are being asked, to travel at their own expense.

Confirmed speakers (topics are tentative)
Sasha Reed - Effects of altered climate of biocrust dominated ecosystems
Anita Antoninka – Determining how best to deploy biocrust inoculum for restoration
Deb Neher – Climate change effects on biocrust fauna
Kyle Doherty – Development of a biocrust moss inoculum for restoration purposes
Jayne Belnap – Review of Chinese language studies of biocrust restoration
Matthew Bowker – 8 years of biocust succession and recovery after nutrient supplements
Eva Dettweiler- Robinson - The Contribution of Biological Soil Crust Carbon and Nitrogen Exchange to the Net Ecosystem Exchange Along an Elevation Gradient
Anny Chung- TBD
Ferran Garcia-Pichel or grad student- TBD
Trent Northen –TBD
Zachary Aanderud – Evaluating Post-Fire Recovery of Biocrusts and Ecosystem Services
Eoin Brodie –
Cheryl Kuske -
Lindsay Chiquoine – update on restoration of gypsum communities
Aindrila Mukhopadhyay -

Possible speakers (pending funds & lifting of federal travel restrictions)
Kirsten Coe
Nichole Barger

Co-Organizers:
Dr. Matthew Bowker, School of Forestry, Northern Arizona University, 200 E Pine Knoll Drive, Northern Arizona University, Flagstaff, AZ 86011. Matthew.bowker@nau.edu

Kyle Doherty, Department of Biological Sciences, Northern Arizona University, Box 5640, Flagstaff, AZ 86011. Kd498@nau,edu.

Trent Northen, Lawrence Berkeley National Lab, One Cyclotron Road , Mailstop: 84R0171, Berkeley, CA 94720, trnorthen@lbl.gov

Call for photos: global soil biodiversity atlas

Dear fellow biocrust fans...this is something that we should all attempt. It would be a shame if soil crusts were not well represented here.

The New Testament is on it's way

Remember this thing? Hopefully every biocrust enthusiast has one on their shelves. Mine is signed by Jayne, and I need to remember to bring it to Spain to collect autographs of Otto Lange and all the other contributors. Of course there were plenty of seminal papers and some pretty good reviews before, but this book (1st edition 2001) has become such a valuable one stop shopping source for crust information that many people have taken to referring to it as the crust bible.

Well, alot has happened since this publication. First, there's just more biocrust researchers which has alot to do with the publication of the crust bible. The subject matter of crust research has changed, for example we are now seeing biocrusts used as model organisms in ecology and more and more climate change research, and we are seeing more and more work on ecological restoration. The geography of the biocrust research community has shifted also. At the time this book was written, biocrust researchers were primarily based in the US, Germany, Israel, and Australia. Now, I think its fair to say that China accounts for at least half if not more of the biocrust research production. Also the emergence of biocrust research in Spain has also been impactful, and a sizable group based in France is also notable. Basically, many more people in many more places are contributing to the biocrust knowledge base. This is undeniably a good thing, but it means that the crust bible is a bit out of date. It needs and update, but more than that.....a sequel. A New Testament!

While there will be several contributors in common, the new book seems to be a bit of a youth movement. Some of the students of the original authors will contribute, in additional to several new contributors. Below is an outline as it stands now. I love the title. To me there seems to be a thinly veiled message: this is an extremely important thing that most of you desert scientists are not noticing, look down once in a while (eyes rolling).

Ecological Studies

Biological Soil Crusts: An Organizing Principle in Drylands

Ed. by B. Weber, B. Büdel and J. Belnap

Table of Contents

Part I: Introduction  

1 Biological soil crusts as a critical zone of global importance (J. Belnap, <jayne_belnap@usgs.gov>)

In this chapter, the concept of biocrusts as the critical zone in drylands will be presented. As these communities cover the soil surface in these regions, they mediate almost all materials entering and leaving the soil, thereby influencing most ecosystem processes including, hydrology, erosion protection, nutrient cycling, vascular plant nutrition and community composition. Their role in ecosystem services will be introduced in this opening chapter.

2 How biological soil crusts became studied as a community (O.L. Lange, <ollange@botanik.uni-wuerzburg.de>)

In this chapter, Professor Lange will describe the history of the first research on biocrusts: the recognition of the organisms as a community, the people who studied them and the techniques utilized.

Part II: Morphology, composition, and distribution of biological soil crusts at different scales

3 Fossil crusts: (H. Beraldi, <hberaldi@unam.mx>)

Biological soil crusts and their components have been identified as fossils from a wide range of rock types found in different parts of the world. In this chapter, these fossil findings will be described and their implications for the evolution of biocrusts and their components will be discussed.

4 Cyanobacteria and algae within biological soil crusts (B. Büdel, <buedel@rhrk.uni-kl.de>)

The diversity and functional roles of cyanobacteria and algae within biocrusts of different (climatic) regions will be described in this chapter. Reasons for variation and stability of taxonomic composition, as well as present and future determination methods will be discussed.

5 Fungi and bacteria within biological soil crusts (M. Grube, <martin.grube@uni-graz.at>)

Description of the diversity and functional roles of fungi and bacteria within biocrusts of different types and (climatic) regions. Present and future methods of determination methods will be discussed.

6 Bryophytes within biological soil crusts (H. Kürschner, <kuersch@zedat.fu-berlin.de>)

The diversity and functional roles of biocrust bryophytes in different habitats (soils, climate, vegetation type) will be described in this chapter. Advantages of a molecular approach in bryophyte identification will be discussed.

7 Lichens within biological soil crusts (M. Westberg, <Martin.Westberg@nrm.se>)

Description of the diversity and functional roles of biocrust lichens from different habitats (soils, climate, vegetation type). Advantages of molecular as compared to classical morphological identifcation methods will be discussed.

8 Microfauna within biological soil crusts (B. Darby, <brian.darby@UND.edu>)

Biocrusts are known to constitute an important habitat for microfauna such as nematodes, collembola, mites, springtails and snails. The diversity and potential functional roles of microfauna within biocrusts of different habitats will be described in this chapter.

9 Composition and structure of biological soil crusts (B. Büdel, <buedel@rhrk.uni-kl.de>)

The composition of biocrusts, comprising the organisms described in chapters 5 to 9, is influenced by climatic, pedogenic and successional parameters. This organism composition, but also macro- and microclimatic conditions as well as landuse patterns are known to influence the external morphology of biocrusts. The variation of biocrust composition and morphology and the resulting effects on ecosystem function will be described.

10 Controls on distribution patterns of biological soil crusts at the micro-, macro-, and global scale (M.A. Bowker, <Matthew.Bowker@nau.edu>)

Distribution patterns of biological soil crusts are determined by a variety of different abiotic factors, such as soil structure and chemistry, vegetation, and climate conditions. Distribution patterns will analyzed and described at different scales.

11 Long-term studies on different types of biological soil crusts (J. Belnap, <jayne_belnap@usgs.gov>)

Biocrusts and their components have been monitored at multiple sites for five to twenty years. Their growth, distribution patterns, and response to climate and vegetation changes give important insights into the long-term stability, development and structure of biocrusts.

12 Remote sensing of biological soil crusts at different scales (B. Weber, <b.weber@mpic.de>)

Imaging spectroscopy methods have been utilized to classify biocrusts within different types of remote sensing imagery. Aside from the classification of biocrusts at the macroscale, imaging spectroscopy has been used to differentiate between different types of biocrusts and also different land use intensities have been differentiated by means of remote sensing techniques.

Part III: Functional roles of biological soil crusts

13 Microstructure and weathering processes within biological soil crusts (F. Garcia-Pichel, <ferran@asu.edu>)

Biological soil crust organisms have been shown to influence the microstructure of the soil and cause weathering processes within the upper soil matrix. These processes, depending on the type of biocrust organisms present, as well as the initial soil composition and structure, will be described in this chapter.

14 Nitrogen cycling of biological soil crusts at micro- macro-, and global scales (N. Barger, <Nichole.Barger@Colorado.EDU>)

Many cyanobacteria and cyanobacterial lichens in biocrusts fix atmospheric nitrogen. This newly fixed nitrogen has three pathways: some is nitrified or denitrified within the biological soil crust, some is leached into underlying soils, and a third part is released into the atmosphere as NO and N₂O. The different sinks of biocrusts have been shown to differ among them, depending on the N-content of the soil, temperature, soil texture and water status. New studies at the global, ecosystem and micro-scales will be presented. Future research methods and questions regarding this highly relevant field of research will also be analyzed.

15 Carbon budgets of biological soil crusts at micro- macro-, and global scales (L. Sancho, <sancholg@farm.ucm.es>)

During the last few years there have been several long-term studies determining the C-budget of biocrusts at the micro- and the mesoscale. These investigations have been conducted at sites within different climatic regions and on several continents. Synthesizing these data promises a big step towards more precise calculations of long-term nutrient fluxes. Apart from these field studies, a global modelling analysis of C-fixation accomplished by biocrusts will be presented in this chapter.

16 Biological soil crusts as soil stabilizers (J. Belnap, <jayne_belnap@usgs.gov>)

Where the biomass of biocrusts is sufficient, they stabilize soils, decreasing both wind and water erosion. They also capture dust, which contains nutrients. Thus, in addition to fixing nitrogen (Chap 14) and carbon (Chap 15) they influence soil fertility in other ways

17 Effects of biological soil crusts on arid land hydrology (S. Chamizo, <scd394@ual.es>)

Biological soil crusts are well-known to affect soil hydrology of arid lands in a complex and non-uniform manner. The effect of biocrusts on infiltration and runoff appear dependent on crust composition, external morphology, soils, site characteristics (e.g., slope), vegetative cover, and macroclimatic conditions. During the last decade, there have been many new insights, which will be presented here.

18 Response of biological soil crust organisms to light, temperature, and water conditions (T.G.A. Green, <greentga@waikato.ac.nz>)

Biocrusts consist of poikilohydric organisms, which passively outlast dry conditions to resurrect again upon favourable water conditions. During the last years they have been shown to adapt to varying light, water and temperature conditions within their environment. Their ability to adapt seems to depend on the overall plasticity of individual crust organisms. The great variability in adaptation potential of different crust organisms will be discussed here.

Part IV: Interactions between biological soil crusts and vascular plants

19 Interactions of biological soil crusts with vascular plants (Y. Zhang, <zhangym@ms.xjb.ac.cn>)

Whereas a nutrient transfer between biocrusts and vascular plants has been assumed in many studies, evidence proving this has only recently been obtained. Several studies have now shown that both C and N can be moved from biocrusts to plants and from plants to biocrusts via fungal hyphae.

Aside from this nutrient transfer, biocrusts have been shown to affect seed retention, germination and plant emergence of vascular plants. Plants adapted to biological soil crust habitats were observed to have smooth seeds (thus lacking appendages), which may facilitate their ability to slip into cracks in the biocrusts. Thus, biological soil crusts have a profound impact on plant structure and communities within arid environments.

20 Biological soil crusts as model to study plant interactions and functional roles (F. Maestre, <fernando.maestre@urjc.es>)

In this chapter, the authors explore how biocrusts of deserts and many other ecosystems may serve as a useful model system for studying multiple questions of interest in community and ecosystem ecology, including biodiversity-ecosystem function relationships, the interplay between positive and negative interactions along environmental gradients, the source-sink hydrological dynamics in drylands, and the role of attributes of biotic communities as modulators of ecosystem responses to global environmental change. To illustrate their views, they synthesize recent and ongoing studies. They complete the synthesis of the studies conducted so far with recommendations for promoting the use of biocrusts by community and ecosystem ecologists, and with a list of priorities for future research on this topic.

Part V: Threats to biological soil crusts

21 Effects of surface disturbance on biological soil crusts (E. Zaady, <zaadye@volcani.agri.gov.il>)

Surface disturbances (e.g., mechanical disturbance, herbicides, fire) all can have severe effects on biological soil crust composition and its physiological activity. Studies of these effects will be discussed in this chapter.

Herbicides, functioning as photosynthesis inhibitors, have been shown to kill cyanobacteria and soil algae, resulting in a decrease in polysaccharide production and biomass.  This, in turn, can lead to a reduction in organic matter and increased soil and nutrient loss through erosion. The detrimental effects of herbicides on biocrusts will be investigated on different time-scales within this chapter.

22 Effects of climate change on biological soil crusts (S. Reed, <screed@usgs.gov>)

The effects of climate change on biological soil crusts are expected to be complex. An increase in temperature will reduce soil moisture, especially at the soil surface. Future changes in precipitation amount and patterns will vary between different regions. In areas with fewer precipitation events and lower total amounts of rainfall, biological soil crust coverage is expected to decrease and composition is predicted to shift towards more early-successional biocrust types. As most processes (e.g., nitrogen and carbon fixation) are temperature and moisture dependent, these will be affected as well. On the other hand, arid and semi-arid regions are known to expand and the increased melting rate of glaciers exposes bare soil surfaces, which serve as an ideal habitat for biocrusts to colonize. Thus, the effects of climate change on biocrusts are expected to be variable.

Part VI: Natural and Enhanced Recovery and Management

23 Natural recovery of biological soil crusts after disturbance (B. Weber, <b.weber@mpic.de>)

Natural recovery of biological soil crusts after disturbance has been studied both in descriptive and experimental studies. Whereas many investigations have shown that biocrusts need decades, if not centuries, to completely recover after disturbance, other studies reveal that biocrusts show significant recovery after only a few years. In this chapter, we will examine the data to find the factors (e.g., crust composition, soil, climate, disturbance type) that predict recovery rates.   

24 Enhanced recovery of biological soil crusts after disturbance (Y. Zhao, <zyunge@ms.iswc.ac.cn>)

Different methods to enhance biological soil crust recovery after disturbance have been experimentally investigated. These have included stabilization of the soil surface with polyacrylamide gels, inoculation of disturbed sites with cyanobacterial cultures or field-collected material, and shade structures. These efforts have been differentially successful, and factors leading to success will be discussed.

Part VII: Future Research on biological soil crusts

25 Synthesis on biological soil crust research (B. Weber, <b.weber@mpic.de>)

In the final synthesis chapter, we will summarize the essential new findings regarding the different topics of biocrusts. Additionally, we will identify knowledge gaps and promising new fields of research. We will call for unified approaches to biocrust research and linking of researchers and sites in order to answer pressing questions. 

IAB blog: IAB 2013 London, UK

IAB blog: IAB 2013 London, UK: --> IAB 2013 London, UK From Jeff Duckett,   Silvia Pressel and Jo Wilbraham We are pleased to announce that the next mee...

BIOCRUST 2013 (Madrid) Third Circular, get your abstracts in by Dec. 31

Below is the latest on the biocrust meeting in Spain next year. I've been told that over 30 abstracts have been received so far. The deadline was extended to 31 December.  Also the plenary talks are now scheduled, and I'm happy to be doing one of them:

Third circular, 12 December 2012

We are pleased to announce the Second International Workshop on Biological Soil Crust, which follows the successful first Workshop celebrated in Germany in 2010. This workshop is devoted to disseminate recent advances in our knowledge of the ecology of biological soil crusts (BSCs) and their importance as a key driver of ecosystem structure and functioning.

The main objective of this Workshop is to trigger an exchange of ideas and results, to discuss possible new theories/approaches, and to provide a forum to facilitate the collaboration among the growing international community of scientists working with BSCs.

This international meeting will take place at the Faculty of Pharmacy, The Complutense University, Madrid, Spain, between 10th and 13rd of June, 2013. The meeting will cover any aspect related to BSCs, including the following topics:
• Diversity, ecology and biogeography of BSCs
• Mapping, monitoring and management of BSCs
• Role of BSCs in ecosystems
• Taxonomy of BSC constituents
• Disturbance and restoration of BSCs
• Interaction between BSCs and vascular plant vegetation
• Effects of global environmental change on BSCs

The meeting will include invited plenary talks, contributed oral sessions, poster sessions, a field trip and some open, informal sessions to facilitate the exchange of ideas and protocols on key issues surrounding BSC ecology.
 

Venue
The Complutense University (http://portal.ucm.es/en/web/en-ucm) is one of the largest Universities in Spain. Located in the historic Ciudad Universitaria/Moncloa Campus, it is easily accessible from anywhere in Madrid from Metro and Bus. The venue of the meeting (Faculty of Pharmacy) is just 20 m from a metro station.
 

Scientific committee
Jayne Belnap, United States Geological Service (USA)
Matthew A. Bowker, Northern Arizona University (USA)
Burkhard Büdel, University of Kaiserslautern (Germany)
David Eldridge, University of New South Wales (Australia)
Ferran García-Pichel, Arizona State University (USA)
Fernando T. Maestre, Rey Juan Carlos University (Spain)
Leopoldo G. Sancho, Complutense University (Spain)
Eli Zaady, Ministry of Agriculture (Israel)
Local organizing committee
Beatriz Gozalo, Rey Juan Carlos University
Allan Green, Complutense University
Fernando T. Maestre, Rey Juan Carlos University
José Raggio, Complutense University
Victoria Ochoa, Rey Juan Carlos University
Ana Pintado, Complutense University
Mª Dolores Puche, Rey Juan Carlos University
Leopoldo G. Sancho, Complutense University
 

Program
10.6. Arrival, registration, workshop sessions (morning and afternoon).

11.6. Workshop sessions (morning and afternoon).

12.6. Field trip to the Guadarrama Mountain Range (8:00 – 16:00 h). Informal discussion 

session in a field station in the mountains (16:00 – 18:00 h). Conference dinner in the Botanical Gardens of the University.

13.6. Workshop sessions (morning), departure after lunch.
 

Plenary speakers are now confirmed (the title of the talks is tentative):
Dr. Matthew A. Bowker, Assistant Professor, Northern Arizona University. Topic of his talk: “Biological soil crusts as a model system on community and ecosystem ecology”. 

Dr. Burkhard Büdel, Professor, University of Kaiserslautern. Topic of his talk: “Soil Crust InterNational (SCIN) – Understanding and valuing biological soil protection of disturbed and open land surfaces”.

Dr. Steve Pointing, Professor, Auckland University of Technology. Topic of his talk: “Understanding microbial contributions to ecosystem-wide patterns and processes in extreme environments”.

Abstract submission
Abstract submission will be open from 20 September 2012 to 31 December 2012.
Authors are invited to present regular talks, short ideas and/or posters at the meeting. Regular contributions will be talks of 15 minutes + 5 minutes discussion each. Short notes/ideas can be presented in 5 minute talks (+ 3 minutes discussion). Poster sessions will also take place the first two days of the meeting.

For all the contribution types, please submit abstracts by e-mail (to iibscworkshop@gmail.com) using this template and indicate, if you wish to present a regular contribution, a short note or a poster. Please note that the number of slots available for regular and short talks is limited, and we may not be able to accommodate all the requests for talks we may have.
 
The template for the abstract can be found available in the webpage of the meeting.
 
Registration and fees
The registration will be open from 1 January 2013 to 30 April 2013.
Conference fees:
240 € regular participants
120 € students

The fees include the documentation, the lunches of three days, the field trip and the conference dinner. Payment of the fees will be done by either credit card or bank transfer, using the registration form available here and in the webpage of the meeting. Once filled in you must submit the form directly by fax or e-mail to the General Foundation UCM (e-mail address and fax number are in the template). Please do not send it to us.
 
Travel Information
Madrid, the Spanish capital, is a vibrant city with world class museums, monuments, and restaurants, and with a famous night and cultural life. Madrid can be easily reached by plane from anywhere in the world. Flights arrive to Barajas airport, from where the city centre can be reached by metro, train ("Cercanías"), bus or taxi. The best way to arrive to the meeting from the city center is by Metro or bus. A metro map and travel itinerary planner can be found here.

Participants are free to book the accommodation of their choice, as there are plenty of options within Madrid, from cheap hostels to luxury hotels. We are making arrangements with a travel agency, which will offer some hotels at a discounted price for participants. We will update details on how to book through them in the next circular.
 
For general travelling and tourism information please visit:
http://www.esmadrid.com/en/portal.do (Touristic information on Madrid and schedule of cultural events going out in the city)
http://www.spain.info/en_US/ (General touristic information)
http://www.aena.es/csee/Satellite/Home/en/Page/1166792871783/ (Information on flights going to the Barajas airport, the main airport in Madrid)
Important dates
 
Abstract submission: Abstract submission will be from 20 September 2012 to 31 December 2012.
Notification of abstract acceptance: 30 January 2013
Registration: 1 January 2013 – 30 April 2013
Workshop: 10 – 13 June 2013
We hope to see you all at Madrid in 2013!
Fernando T. Maestre (fernando.maestre@urjc.es) and Leopoldo G. Sancho (sancholg@farm.ucm.es)