Microbial production of recalcitrant dissolved organic matter: long-term carbon storage in the global ocean
The biological pump is a process whereby CO2 in the upper ocean is fixed by primary
producers and transported to the deep ocean as sinking biogenic particles or as dissolved …
producers and transported to the deep ocean as sinking biogenic particles or as dissolved …
Oxygenation, life, and the planetary system during Earth's middle history: An overview
The long history of life on Earth has unfolded as a cause-and-effect relationship with the
evolving amount of oxygen (O2) in the oceans and atmosphere. Oxygen deficiency …
evolving amount of oxygen (O2) in the oceans and atmosphere. Oxygen deficiency …
The tempo of Ediacaran evolution
The rise of complex macroscopic life occurred during the Ediacaran Period, an interval that
witnessed large-scale disturbances to biogeochemical systems. The current Ediacaran …
witnessed large-scale disturbances to biogeochemical systems. The current Ediacaran …
The geologic time scale
Construction and assembly of the Geologic Time Scale involves:(a) constructing a relative
(chronostratigraphic) standard scale for key periods in the Earth's rock record;(b) identifying …
(chronostratigraphic) standard scale for key periods in the Earth's rock record;(b) identifying …
The Neoproterozoic oxygenation event: Environmental perturbations and biogeochemical cycling
The oxygen content of the Earth's surface environment is thought to have increased in two
broad steps: the Great Oxygenation Event (GOE) around the Archean–Proterozoic boundary …
broad steps: the Great Oxygenation Event (GOE) around the Archean–Proterozoic boundary …
Ferruginous conditions dominated later Neoproterozoic deep-water chemistry
Earth's surface chemical environment has evolved from an early anoxic condition to the oxic
state we have today. Transitional between an earlier Proterozoic world with widespread …
state we have today. Transitional between an earlier Proterozoic world with widespread …
A stratified redox model for the Ediacaran ocean
The Ediacaran Period (635 to 542 million years ago) was a time of fundamental
environmental and evolutionary change, culminating in the first appearance of macroscopic …
environmental and evolutionary change, culminating in the first appearance of macroscopic …
Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation (ca. 635–551 Ma) in south China
The Ediacaran Doushantuo Formation (ca. 635–551Ma) in South China contains
exceptionally well-preserved fossils of multicellular eukaryotes including early animals, and …
exceptionally well-preserved fossils of multicellular eukaryotes including early animals, and …
Fossil steroids record the appearance of Demospongiae during the Cryogenian period
Abstract The Neoproterozoic era (1,000–542 Myr ago) was an era of climatic extremes and
biological evolutionary developments culminating in the emergence of animals (Metazoa) …
biological evolutionary developments culminating in the emergence of animals (Metazoa) …
Ocean oxygenation in the wake of the Marinoan glaciation
Metazoans are likely to have their roots in the Cryogenian period,,, but there is a marked
increase in the appearance of novel animal and algae fossils shortly after the termination of …
increase in the appearance of novel animal and algae fossils shortly after the termination of …