Structural details of the crust play an important role in controlling the distribution of volcanic activity in arc systems. In southwest Washington, several different regional structures associated with accretion and magmatism have been invoked to explain the broad distribution of Cascade volcanism in this region. In order to image these regional structures in the upper crust, Pg and Sg travel times from the imaging Magma Under St. Helens (iMUSH) active‐source seismic experiment are inverted for
Chiral groups induce opposite twist senses of
- Publication Date:
- NSF-PAR ID:
- 10075169
- Journal Name:
- Chemical Science
- ISSN:
- 2041-6520
- Publisher:
- Royal Society of Chemistry (RSC)
- Sponsoring Org:
- National Science Foundation
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Abstract V p ,V s , andV p /V s models in the region surrounding Mount St. Helens. Several features of these models provide new insights into the regional structure of the upper crust. A large section of the Southern Washington Cascades Conductor is imaged as a lowV p /V s anomaly that is inferred to represent a broad sedimentary/metasedimentary sequence that composes the upper crust in this region. The accreted terrane Siletzia is imaged west of Mount St. Helens as north/south trending highV p andV p /V s bodies. TheV p /V s model shows relatively highV p /V s regions near Mount St. Helens and the Indian Heaven Volcanic Field, which could be related to the presence of magmatic fluids. Separating these two volcanic regions below 6‐km depth is a northeast trending series of highV p andV s bodies. These bodies have the same orientation as several volcanic/magmatic features at the surface, including Mountmore » -
Abstract Ocean transform faults often generate characteristic earthquakes that repeatedly rupture the same fault patches. The westernmost Gofar transform fault quasi‐periodically hosts ∼
M 6 earthquakes every ∼5 years, and microseismicity suggests that the fault is segmented into five distinct zones, including a rupture barrier zone that may have modulated the rupture of adjacentM 6 earthquakes. However, the relationship between the systematic slip behavior of the Gofar fault and the fault material properties is still poorly known. Specifically, the role of pore fluids in regulating the slip of the Gofar fault is unclear. Here, we use differential travel times between nearby earthquakes to estimate the in‐situV p /V s of the fault‐zone materials. We apply this technique to the dataset collected by an ocean‐bottom‐seismometer network deployed around the Gofar fault in 2008, which recorded abundant microearthquakes, and find a moderateV p /V s of 1.75–1.80 in the rupture barrier zone and a lowV p /V s of 1.61–1.69 in the down‐dip edge of the 2008M 6 rupture zone. This lateral variation inV p /V s may be caused by both pore fluids and chemical alteration. We also find a 5%–10% increase inV p /V s in the barrier zone during the 9 months before the mainshock. This increase may have been caused by fluid migrations or slip transients in the barrier zone. -
The marine diazotroph
Crocosphaera watsonii provides fixed carbon (C) and nitrogen (N) to open‐ocean regimes, where nutrient deficiency controls productivity. The growth ofCrocosphaera can be limited by low phosphorus (P) concentrations in these oligotrophic environments. Biomarkers such as the high‐affinityABC transporter phosphate‐binding gene,pstS , are commonly used to monitor when such organisms are under P stress; however, transcriptional regulation of these markers is often complex and not well‐understood. In this study, we interrogated changes inpstS transcript levels inC. watsonii cells under P starvation, and in response to added dissolved inorganic phosphorus (DIP ), dissolved organic phosphorus (DOP ), and changing light levels. We observed elevated relativepstS transcript levels inC. watsonii WH 8501 atDIP concentrations below 60 and above 20 nmol · L−1. Transcript levels were suppressed by both inorganic and bioavailable organic phosphorus; however, the P stress response was more sensitive toDIP thanDOP sources. Increasing light intensity resulted in increased relativepstS transcript abundances independently of low external P, and seemed to exacerbate the physiological effects of P stress. The variable response to different P compounds and rapid and transient influence of high light onpstS transcript abundances suggests thatpstS is an indicator of internal P status inCrocosphaera . -
Since the first phylogenetic study of the order Batrachospermales,
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