Microbial structures in Neoproterozoic cap carbonates record the environmental processes present in the aftermath of global glaciation. The Rasthof Formation of northern Namibia is a unique carbonate depositional sequence that formed during post-glacial transgression and highstand following the Chuos glaciation. Carbon isotope profiles from four examined localities reveal that onlap was diachronous over post-glacial, syn-rift topography. The lower Rasthof Formation consists primarily of dark gray thinly (<mm) and thickly (1–4 mm) laminated microbialites that exhibit different rheological responses to the emplacement of syndepositional dikes. The thinly laminated microbialaminite facies commonly host cm-sized syndepositional folds of microbi...
Evidence for glaciation during the mid-late Neoproterozoic is widespread on Earth, reflecting three ...
Cap carbonates of Cryogenian age may contain insights into the previously scarce fossil record of on...
The study of microbial carbonates has acquired new significance with the recognition that they retai...
During the Neoproterozoic Era, there is extensive geochemical, sedimentological and paleomagnetic ev...
Laminated carbonates of the Rasthof Formation, deposited in the aftermath of the early Cryogenian lo...
Cryogenian cap carbonates that overlie Sturtian glacial deposits were formed during a post‐glacial t...
Laminated carbonates of the Rasthof Formation, deposited in the aftermath of the early Cryogenian lo...
In the late Neoproterozoic (~750 to 635 Ma), geochemical, paleomagnetic, and sedimentological eviden...
Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose n...
Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose n...
Paleomagnetic data suggest that the early Cryogenian (Sturtian) glaciation extended to sea level at ...
The Neoproterozoic Cryogenian (‘Marinoan’) Ghaub Formation of northwestern Namibia represents an imp...
The middle Neoproterozoic carbonate-dominated uppermost Haut-Shiloango Subgroup (Sh8h and Sh8i membe...
The carbon isotope geochemistry of carbonates and organic carbon in the late Proterozoic Damara Supe...
The termination of the Marinoan Snowball Earth glacial epoch was one of the most extreme climate eve...
Evidence for glaciation during the mid-late Neoproterozoic is widespread on Earth, reflecting three ...
Cap carbonates of Cryogenian age may contain insights into the previously scarce fossil record of on...
The study of microbial carbonates has acquired new significance with the recognition that they retai...
During the Neoproterozoic Era, there is extensive geochemical, sedimentological and paleomagnetic ev...
Laminated carbonates of the Rasthof Formation, deposited in the aftermath of the early Cryogenian lo...
Cryogenian cap carbonates that overlie Sturtian glacial deposits were formed during a post‐glacial t...
Laminated carbonates of the Rasthof Formation, deposited in the aftermath of the early Cryogenian lo...
In the late Neoproterozoic (~750 to 635 Ma), geochemical, paleomagnetic, and sedimentological eviden...
Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose n...
Foraminifera are an ecologically important group of modern heterotrophic amoeboid eukaryotes whose n...
Paleomagnetic data suggest that the early Cryogenian (Sturtian) glaciation extended to sea level at ...
The Neoproterozoic Cryogenian (‘Marinoan’) Ghaub Formation of northwestern Namibia represents an imp...
The middle Neoproterozoic carbonate-dominated uppermost Haut-Shiloango Subgroup (Sh8h and Sh8i membe...
The carbon isotope geochemistry of carbonates and organic carbon in the late Proterozoic Damara Supe...
The termination of the Marinoan Snowball Earth glacial epoch was one of the most extreme climate eve...
Evidence for glaciation during the mid-late Neoproterozoic is widespread on Earth, reflecting three ...
Cap carbonates of Cryogenian age may contain insights into the previously scarce fossil record of on...
The study of microbial carbonates has acquired new significance with the recognition that they retai...