English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

) in young to oldplume waters. We first mapped the spatial distribution of hydrothermal plumes by towing a fixed array of optical sensors(Miniature Autonomous Plume Recorders: MAPRs) above the field. We then made water column observations and samplingsusing a CTD (Conductivity, Temperature, and Depth sensors)-Carousel package with a transmissometer and Niskin-Xbottles at five locations, with distances between 0.6 and 6.1 km from the hydrothermally active center so far discovered.Vertical profiles of light transmission and chemical tracers indicated triple-layered plumes, the centers of which were atdepths of 700–800 m, ~1,050 m and ~1,200 m. The CH

Microbial carbon isotope fractionation to produce extraordinarily heavy methane in aging hydrothermal plumes over the southwestern Okinawa Trough