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2019, Frontiers for young minds
https://doi.org/10.3389/frym.2019.00112…
8 pages
1 file
Microbialites are rock-like underwater structures that look like reefs but are made entirely of millions of microbes. These structures are very ancient and can be found in dierent environments on every continent on Earth. Mexico has many microbialite reefs, in desert valleys, crater-lakes, and coastal lagoons. Science helps us to understand the microbes that build microbialites, to know whether the same kinds of microbes make up microbialites in dierent regions of the world, and to figure out how the microbes organize into microbialites. Many things are damaging microbialites in Mexico, including poorly planned development, pollution from lack of sewage treatment, too much water usage, and the fertilizers used for agriculture. Policies that regulate development are urgently needed to help save these diverse and ancient microbial reefs.
BIO Web of Conferences, 2014
Microbialites are sedimentary formations that are found throughout the geological record and are usually considered as one of the oldest traces of life on Earth. Although they have been known for more than a century and hold as an emblematic object in Earth Sciences, we yet do not understand in details how they form and how microbial processes impact their chemistry, structure and macroscopic morphology. Here, we show recent advances achieved owing to funding provided by the EPOV program on the formation of modern microbialites in the crater Lake Alchichica (Mexico). We first show that very diverse microbial communities populate these microbialites, including diverse microbial groups able to induce carbonate precipitation. We demonstrate that this microbial diversity can be preserved for several years in laboratory aquaria offering a nice opportunity for future studies to assess the relationships between biodiversity and microbialite formation. We then detail the textural modifications affecting cyanobacterial cells during the first steps of fossilization as captured in Alchichica microbialites. Finally, we report the discovery of a new deepbranching cyanobacterium species, Candidatus Gloeomargarita lithophora, able to form intracellular Ca-, Mg-, Sr-and Ba-rich carbonates and discuss the implications for the interpretation of the fossil record.
American Journal of Science, 2005
This paper is dedicated to Dr. Terry J. Beveridge, mentor and friend, on the occasion of his 60th birthday. ABSTRACT. Earth's geosphere is intimately tied to its biosphere. A major link between the two lies in the microbial realm; microorganisms grow in and upon rocks and minerals, often relying on their substratum for critical compounds needed in order to produce cellular energy. The presence of a metabolizing cell on a mineral substrate has a significant effect on the mineral texture and on the geochemistry of the surrounding microenvironment. In nature, microorganisms exist in microbial communities as mats or biofilms growing upon a solid substrate. As such they cover a vast surface area both within and below the surface of Earth's land and sea. The following review will provide a glimpse into the latest findings in the field of geomicrobiology and is intended to convey a sense of the profound influence microorganisms can have upon the geological environment they inhabit.
Microbialites are organogenic deposits formed as the result of the vital activities of colonies of benthic micro organisms, which entrap and bind sedimentary particles to form mineral deposits. This article considers two types of such structures: layered (stromatolites, biofilms) and detached formations (thrombolites, oncolites, etc.). The mechanisms and conditions of their development and evolution in the history of the Earth are shown. At present, integrated studies on microbialites are becoming an important subdiscipline of lithology.
Advances in Stromatolite Geobiology, 2011
Laguna Bacalar, a karstic freshwater lake in the state of Quintana Roo, Yucatan Peninsula, Mexico (Fig. 1) features in its southern part possibly the largest freshwater microbialite structures known. These structures extend continuously for over 10 km (Gischler et al. 2008). The laguna is a narrow, elongated body of freshwater, about 40 km long and 1–2 km wide, extending NE to SW with an adjacent strip of periodically flooded lowland. The lagoon is tectonically rooted on the Bacalar fault, which is the northern continuation of the Rio ...
Geobiology, 2013
Microbialites are the most abundant macrofossils of the Precambrian. Decline in microbialite abundance and diversity during the terminal Proterozoic and early Phanerozoic has historically been attributed to the concurrent radiation of complex metazoans. Similarly, the apparent resurgence of microbialites in the wake of Paleozoic and Mesozoic mass extinctions is frequently linked to drastic declines in metazoan diversity and abundance. However, it has become increasing clear that microbialites are relatively common in certain modern shallow, normal marine carbonate environments-foremost the Bahamas. For the first time, we present data, collected from the Exuma Cays, the Bahamas, systematically characterizing the relationship between framework-building cyanobacteria, microbialite fabrics, and microbialite-associated metazoan abundance and diversity. We document the coexistence of diverse microbialite and infaunal metazoan communities and demonstrate that the predominant control upon both microbialite fabric and metazoan community structure is microbial mat type. These findings necessitate that we rethink prevalent interpretations of microbialite-metazoan interactions and imply that microbialites are not passive recipients of metazoan-mediated alteration. Additionally, this work provides support for the theory that certain Precambrian microbialites may have been havens of early complex metazoan life, rather than bereft of metazoans, as has been traditionally envisaged.
Goldschmidt2021 abstracts, 2021
Geobiology, 2018
The formation of the microbially influenced organosedimentary carbonate deposits known as microbialites has been shown to result from the interplay of microbial cells, their metabolisms, and the chemistry of their environment (see Riding, 2000). This microbial influence can be physically or chemically mediated and can be either active or passive in character (Burne & Moore, 1987; Dupraz et al., 2009). Microbialites are often classified by their petrographic texture, those with laminations being stromatolites and those with
PLOS ONE, 2020
Microbialites are highly diverse microbial communities that represent modern examples of the oldest life forms, stromatolites (dated >3.7 Ga). Bacalar Lagoon, in Mexico, harbors the largest freshwater microbialite occurrences of the world; yet diverse anthropogenic activities are changing the oligotrophic conditions of the lagoon. The objective of this work was to perform a spatial exploration of the microbialites of Bacalar Lagoon, analyze their prokaryote diversity, following a high throughput sequencing approach of the V4 region of the 16S rDNA, and correlate to the environmental parameters that influence the structure of these communities. The results indicate the presence of microbialites throughout the periphery of the lagoon. The microbiome of the microbialites is composed primarily of Proteobacteria (40–80%), Cyanobacteria (1–11%), Bacteroidetes (7–8%), Chloroflexi (8–14%), Firmicutes (1–23%), Planctomycetes (1–8%), and Verrucomicrobia (1–4%). Phylogenetic distance analyses suggests two distinct groups of microbialites associated with regions in the lagoon that have differences in their environmental parameters, including soluble reactive silicate (in the north), bicarbonates and available forms of nitrogen (ammonium, nitrates and nitrites) (in the south). These microbialite groups had differences in their microbiome composition associated to strong anthropogenic pressure on water quality (agriculture, landfill leachate, lack of water treatment infrastructure and intensive tourism), which were related to a loss of microbial diversity.
Geobiology, 2008
The interactions between the geosphere and the biosphere are central questions in environmental and geological research. The relationship between bacteria and their environment is an important example of these interactions. By studying microbial communities in modern environments, it is possible to understand the underlying mechanisms that shape these environments and apply this knowledge to the rock record. Recently, new experimental and theoretical methods, ranging from nano-and biotechnology to mathematical and conceptual modelling, have come into play. Thus, new opportunities for interdisciplinary research in the field of geobiology have emerged. In this paper, we review aspects of state-of-the-art imaging and modelling techniques and propose a research concept linking the experimental and the theoretical approaches. Fig. 5 Sequence of model results showing the surface topography after an increasing number of atomic blocks are removed. The initial surface was flat. The bottom part of the figure shows the surface topography in 3D after 2000 atomic blocks are removed (compare Fig. 5D). REFERENCES Arvidson RS, Ertan IE, Amonette JE, Luttge A (2003) Variation in calcite dissolution rates: a fundamental problem? Geochimica et Cosmochimica Acta 67, 1623-1634. Beveridge TJ (1978) Response of cell-walls of Bacillus subtilis to metals and to electron-microscopic stains. Canadian Journal of Microbiology 24, 89-104. Beveridge TJ (1981) Ultrastructure, chemistry and function of the bacterial wall. International Review of Cytology 72, 229-317.
2017
What is a comic? The simple answer states that a comic is a drawn story that is picture- rather than text-oriented and told serially. In other words, a comic is a type of illustration. Realism is not its goal; rather a narrative is developed through reduction according to specific stylistic means. I start this article with a definition of the term “comic”, and move on to highlight the complexity of the comic and to argue that insight into this complexity is necessary for its correct interpretation. Only then can we recognise that the comic is not only entertaining but also, in its own way, a vehicle for content that might be system confirming and propagandistic but can also be system critical. Doing so allows us to see the potential of the comic that is embedded in its particular affinity with nonlinear interactive audiovisual media.
Η' ΔΙΕΘΝΕΣ ΕΠΙΣΤΗΜΟΝΙΚO ΣΥΝEΔΡΙΟ: ΑΓΙΟΝ ΟΡΟΣ ΚΑΙ ΛΟΓΙΟΣΥΝΗ / MOUNT ATHOS AND SCHOLARSHIP - ΠΡΑΚΤΙΚΑ ΣΥΝΕΔΡΙΟΥ / CONFERENCE PROCEEDINGS, 2014
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