scholarly journals Mineral authigenesis within chemosynthetic microbial mats: Coated grain formation and phosphogenesis at a Cretaceous hydrocarbon seep, New Zealand

2020 ◽  
Author(s):  
Jennifer Zwicker ◽  
Daniel Smrzka ◽  
Florian Steindl ◽  
Michael E. Böttcher ◽  
Eugen Libowitzky ◽  
...  

Zootaxa ◽  
2016 ◽  
Vol 4154 (1) ◽  
pp. 1 ◽  
Author(s):  
KRISTIAN P. SAETHER ◽  
SHA JINGENG ◽  
CRISPIN T. S. LITTLE ◽  
KATHLEEN A. CAMPBELL


Zootaxa ◽  
2010 ◽  
Vol 2577 (1) ◽  
pp. 1 ◽  
Author(s):  
KRISTIAN P. SAETHER ◽  
CRISPIN T. S. LITTLE ◽  
KATHLEEN A. CAMPBELL ◽  
BRUCE A. MARSHALL ◽  
MIKE COLLINS ◽  
...  

Bathymodiolus (sensu lato) heretaunga sp. nov. and Gigantidas coseli sp. nov. are described from Miocene-age hydrocarbon seep carbonates of North Island, New Zealand, adding to only four described fossil hydrocarbon seep mussel species. Both new species are small compared to their modern congeners, and it is suggested that an evolutionary trend toward gigantism occurred in vent and seep mussels since the first known fossil species of the group appeared in the Middle Eocene. Bathymodiolus heretaunga is highly variable in morphology, potentially reflecting population variation over a wide geographic area. Gigantidas coseli is the first named species, fossil or modern, of its genus known from hydrocarbon seeps, although several closely related species in the same group, the Bathymodiolus childressi clade, have been reported from these environments.



2010 ◽  
Vol 33 (3) ◽  
pp. 205-219 ◽  
Author(s):  
M.J. Pearson ◽  
E. Grosjean ◽  
C.S. Nelson ◽  
S.L. Nyman ◽  
G.A. Logan


2017 ◽  
Vol 8 ◽  
Author(s):  
Blair G. Paul ◽  
Haibing Ding ◽  
Sarah C. Bagby ◽  
Matthias Y. Kellermann ◽  
Molly C. Redmond ◽  
...  


2010 ◽  
Vol 55 (3) ◽  
pp. 507-517 ◽  
Author(s):  
Kristian P. Saether ◽  
Crispin T.S. Little ◽  
Kathleen A. Campbell




2008 ◽  
Vol 204 (3-4) ◽  
pp. 83-105 ◽  
Author(s):  
Kathleen A. Campbell ◽  
David A. Francis ◽  
Mike Collins ◽  
Murray R. Gregory ◽  
Campbell S. Nelson ◽  
...  


2003 ◽  
Vol 40 (11) ◽  
pp. 1585-1610 ◽  
Author(s):  
Brian Jones ◽  
Robin W Renaut

Domal masses of geyserite, which surround many geyser vents in the Whakarewarewa geothermal area, are formed largely of spicules, spicule columns, and shrub columns. The non-branching spicules and the branches of branching spicules, individually up to 3 cm high and 1 mm diameter, have a laminated core encased by siliceous cortex. Silicified microbes are rare in the core but common in the cortex. Silicified microbial mats and pseudodendrites are found in the crevices between neighbouring spicules. Shrub columns, up to 5 cm high and 1.5 cm in diameter, are formed of opal-A that was precipitated around a three-dimensional, branching, shrub-like microbial (?) structure. The shrub branches, which are hollow with scalloped walls, do not contain any evidence of the original microbes or minerals that formed them. Silicified microbial mats are present between the columns. Microbial boring and etching by acidic steam led to local diagenetic degradation of these columns. In the geyserite mounds at Whakarewarewa, spicules and spicule columns are common, whereas shrub columns are rare. Interbedding and intercalation of spicular geyserite with shrub columnar geyserite indicate, however, that these different morphologic entities probably formed under similar environmental conditions on the mounds around the geyser vents. Petrographic evidence shows that the spicules, spicule columns, and shrub columns grew through a combination of biotic and abiotic processes.



1999 ◽  
Vol 190 ◽  
pp. 563-566
Author(s):  
J. D. Pritchard ◽  
W. Tobin ◽  
J. V. Clausen ◽  
E. F. Guinan ◽  
E. L. Fitzpatrick ◽  
...  

Our collaboration involves groups in Denmark, the U.S.A. Spain and of course New Zealand. Combining ground-based and satellite (IUEandHST) observations we aim to determine accurate and precise stellar fundamental parameters for the components of Magellanic Cloud Eclipsing Binaries as well as the distances to these systems and hence the parent galaxies themselves. This poster presents our latest progress.



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