'Molar-tooth microspar': a chemical explanation for its disappearance ~ 750 Ma
Shields, Graham A. (2002) 'Molar-tooth microspar': a chemical explanation for its disappearance ~ 750 Ma. Terra Nova, 14 (2). pp. 108-113.
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Molar-tooth structures are intricately crumpled, microsparry calcite fissure fills that formed during the Precambrian. Strontium isotope stratigraphy constrains the last occurrence of volumetrically significant molar-tooth structure (MT) in the geological record to ∼ 750 Ma. Although the disappearance of MT is commonly ascribed to the influence of metazoans on sediment cohesion, this now seems less plausible because there is no evidence for significant sediment disruption by metazoans before ∼ 550 Ma. It is proposed here that the most likely alternative explanation for MT disappearance is a change in ocean chemistry. A decrease in CaCO3 saturation and/or an increase in the concentration of precipitation inhibitors in mid-Neoproterozoic seawater may have contributed to MT disappearance, and might also help to explain the approximately contemporaneous decline in stromatolite diversity.
|Item Type:||Article (Refereed Research - C1)|
|FoR Codes:||04 EARTH SCIENCES > 0402 Geochemistry > 040299 Geochemistry not elsewhere classified @ 100%|
|SEO Codes:||97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%|
|Deposited On:||20 Dec 2010 10:38|
|Last Modified:||12 Feb 2011 20:10|
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