Geology - Pre-Issue Publication
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Coupled oceanic oxygenation and metazoan diversification during the early-middle Cambrian?

The early–middle Cambrian (Fortunian to Age 4) is characterized by a significant increase in metazoan diversification. Furthermore, this interval is marked by a prominent environmental and ecological expansion of arthropod- and echinoderm-rich biotas. Recent redox work has suggested that this shift occurred during stable or decreasing marine oxygen...

Sat Jun 10, 2017 04:52
Fire biases the production of charred flowers: Implications for the Cretaceous fossil record

The radiation of angiosperm lineages during the Cretaceous Period (145.5–65.5 Ma) initiated one of the greatest floral turnovers to have occurred on our planet. Much of our understanding of the floral biology and diversity of these early angiosperms derives from exceptionally preserved charcoalified and coalified Cretaceous fossil floras. Although...

Sat Jun 10, 2017 04:52
Cryptic metasomatism during late-stage lunar magmatism implicated by sulfur in apatite

The use of volatile-bearing (H2O-Cl-F-C-S) minerals as proxies for constraining the volatile content of lunar magmas remains controversial. In this study, we apply published F-Cl-S signature trends in apatite from lunar mare basalts, new experimentally determined apatitemelt partition coefficients for S, and thermodynamic modeling to demonstrate...

Sat Jun 10, 2017 04:52
In situ peridotitic diamond in Indus ophiolite sourced from hydrocarbon fluids in the mantle transition zone

In recent years ophiolitic diamonds have been reported mostly from podiform chromitites. However, the mechanism of such diamond formation remains unknown. We report in situ diamond, graphite pseudomorphs after diamond crystals, and hydrocarbon (C-H) and hydrogen (H2) fluid inclusions in ultrahigh-pressure (UHP) peridotitic minerals of the Nidar...

Sat Jun 10, 2017 04:52
Outgassing and eruption of basaltic magmas: The effect of conduit geometry

The flow dynamics of magmas is controlled by several parameters, including magma rheology, density, surface tension, gas and liquid flow rate, and the geometry of the flow field, which is mainly regulated by the conduit shape. For this reason, magmatic flows along fissures and dikes are significantly different from those along axisymmetric conduits....

Sat Jun 10, 2017 04:52
Tropical weathering of the Taconic orogeny as a driver for Ordovician cooling

The Earth's climate cooled through the Ordovician Period leading up to the Hirnantian glaciation. Increased weatherability of silicate rocks associated with topography generated on the Appalachian margin during the Taconic orogeny has been proposed as a mechanism for Ordovician cooling. However, paleogeographic reconstructions typically place the...

Sat Jun 10, 2017 04:52

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