scholarly journals Frozen Zoo: a collection of permafrost samples containing viable protists and their viruses

2020 ◽  
Vol 8 ◽  
Author(s):  
Stas Malavin ◽  
Lyubov Shmakova ◽  
Jean-Michel Claverie ◽  
Elizaveta Rivkina

Permafrost, frozen ground cemented with ice, occupies about a quarter of the Earth’s hard surface and reaches up to 1000 metres depth. Due to constant subzero temperatures, permafrost represents a unique record of past epochs, whenever it comes to accumulated methane, oxygen isotope ratio or stored mummies of animals. Permafrost is also a unique environment where cryptobiotic stages of different microorganisms are trapped and stored alive for up to hundreds of thousands of years. Several protist strains and two giant protist viruses isolated from permafrost cores have been already described. In this paper, we describe a collection of 35 amoeboid protist strains isolated from the samples of Holocene and Pleistocene permanently frozen sediments. These samples are stored at −18°C in the Soil Cryology Lab, Pushchino, Russia and may be used for further studies and isolation attempts. The collection strains are maintained in liquid media and may be available upon request. The paper also presents a dataset which consists of a table describing the samples and their properties (termed "Sampling events") and a table describing the isolated strains (termed "Occurrences"). The dataset is publicly available through the GBIF portal.

2018 ◽  
Vol 32 (9) ◽  
pp. 703-710 ◽  
Author(s):  
Steven J. Granger ◽  
Yuguo Yang ◽  
Verena Pfahler ◽  
Chris Hodgson ◽  
Andrew C. Smith ◽  
...  

1971 ◽  
Vol 26 (9) ◽  
pp. 1485-1490 ◽  
Author(s):  
K. Heinzinger ◽  
C. Iunge ◽  
M. Schidlowski

Abstract The separation factor, aM-0= (18O/16O) magnetite/' (18O/16O) atmospheric oxygen, between the magnetite crust of iron meteorites and atmospheric oxygen has been determined to be 0.9946 ± 0.0005. It is concluded that this fractionation of the oxygen isotopes is the consequence of an equilibrium isotope effect at high temperatures. It can be assumed that this is also valid for cosmic spherules, which are mainly ablation products of iron meteorites. As these spherules are found in sediments of different geological ages, their oxygen isotope ratio can give information on the development of atmospheric oxygen. The difference of the oxygen isotope ratios between magnetite from the lithosphere and airborne magnetite can be used to distinguish between terrestrial and extraterrestrial material.


2019 ◽  
Vol 526 ◽  
pp. 23-35 ◽  
Author(s):  
Melita Peharda ◽  
Julien Thébault ◽  
Krešimir Markulin ◽  
Bernd R. Schöne ◽  
Ivica Janeković ◽  
...  

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