Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

View all journals
Search
Log in

nature
search

Search

Advanced search

Filter By:

Journal Check one or more journals to show results from those journals only.

Nature Geoscience (1)
Scientific Reports (1)
Communications Earth & Environment (1)

Choose more journals

Article type Check one or more article types to show results from those article types only.

Research (3)

Subject Check one or more subjects to show results from those subjects only.

Biogeochemistry
Climate sciences
Ocean sciences
Solid Earth sciences

Date Choose a date option to show results from those dates only.

Today
Last 7 days
Last 30 days
Last 12 months
Last 2 years
Last 5 years

Custom date range

Clear all filters

Sort by:

Relevance

Date published (new to old)

Date published (old to new)

Showing 1–3 of 3 results

Advanced filters: Author: Hayley R. Manners Clear advanced filters

Late Ordovician climate change and extinctions driven by elevated volcanic nutrient supply

Increased volcanism-related phosphorus delivery to the Late Ordovician ocean helps explain widespread cooling and eutrophication-driven extinctions, as shown by a biogeochemical model incorporating volcanic ash phosphorus and carbon isotope records.

Jack Longman
Benjamin J. W. Mills
Martin R. Palmer
Research02 Dec 2021
Nature Geoscience

Volume: 14, P: 924-929
Uniquely low stable iron isotopic signatures in deep marine sediments caused by Rayleigh distillation

Male Köster
Michael Staubwasser
Susann Henkel
ResearchOpen Access24 Jun 2023
Scientific Reports

Volume: 13, P: 1-11
Subaerial volcanism is a potentially major contributor to oceanic iron and manganese cycles

Subaerial volcanism may provide an important source of micronutrients to the surface ocean through the deposition of iron and manganese rich ash, according to Monte Carlo simulations based on ash composition and eruption volume data.

Jack Longman
Martin R. Palmer
Morgan T. Jones
ResearchOpen Access14 Mar 2022
Communications Earth & Environment

Volume: 3, P: 1-8