The effects of redox conditions on arsenic re-release from excavated marine sedimentary rock with naturally suppressed arsenic release

Author(s):  
Akihide Kamata ◽  
Masato Ueshima ◽  
Hirofumi Sakanakura ◽  
Toshihiko Miura ◽  
Masahiko Katoh
2008 ◽  
Vol 276 (1658) ◽  
pp. 887-892 ◽  
Author(s):  
Felix G Marx

The validity of biological explanations of patterns of palaeodiversity has been called into question owing to an apparent correlation of diversity with the amount of sedimentary rock preserved. However, this claim has largely been based on comprehensive estimates of global marine Phanerozoic diversity, thus raising the question of whether a similar bias applies to the records of smaller, well-defined taxonomic groups. Here, new data on European Caenozoic marine sedimentary rock outcrop area are presented and compared with European occurrences of three groups of marine mammals (cetaceans, pinnipedimorphs and sirenians). Limited evidence was found for a correlation of outcrop area with marine mammal palaeodiversity. In addition, similar patterns were identified in the cetacean and pinnipedimorph diversity data. This may point to the preservation of a genuine biological signal not overwhelmed by geological biases in the marine mammal diversity data, and opens the door to further analyses of both marine mammal evolution and geological bias in other small and well-defined groups of taxa.


Paleobiology ◽  
2008 ◽  
Vol 34 (1) ◽  
pp. 155-161 ◽  
Author(s):  
Andrew B. Smith ◽  
A. J. McGowan

It has recently been argued that barren intervals of marine sedimentary rock are less common in the Cenozoic than in the Paleozoic, and that this arises as a direct consequence of widespread epeiric seas and the prevalence of dysaerobic conditions at such times. We show, using an independent and more direct measure of rock outcrop through time in western Europe, that barren marine sedimentary rocks do become less frequent toward the present, but that this is not linked to any epeiric-seas effect. The proportion of barren to fossiliferous rock outcrop correlates well with the inferred Phanerozoic marine diversity curve (although more so in the Paleozoic than in the post-Paleozoic), and shows no correlation or only a weak negative correlation with area over which the sediments have been deposited. We therefore concluded that the Phanerozoic trend in fossiliferousness most likely records the degree to which space is occupied in the shallow marine realm.


2021 ◽  
Author(s):  
Juraj Farkas ◽  
Robert Klaebe ◽  
Geremiah Toledo ◽  
Jessica Stromberg ◽  
Sam Spinks ◽  
...  

2005 ◽  
Vol 1 (4) ◽  
pp. 443-445 ◽  
Author(s):  
Andrew B Smith ◽  
Alistair J McGowan

In a recent article, Rohde & Muller (Rohde & Muller 2005 Nature 434 , 208–210) identified a strong 62 Myr cyclicity in the history of marine diversity through the Phanerozoic. The data they presented were highly convincing, yet they were unable to explain what process might have generated this pattern. A significant correlation between observed genus-level diversity (after removal of long-term trends) and the amount of marine sedimentary rock measured at a surface outcrop in Western Europe is demonstrated. This suggests that cyclicity originates from long-term changes in sedimentary depositional and erosional regimes, and raises the strong possibility that the cyclicity apparent in the record of marine fossils is not a biological signal but a sampling signal.


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