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sediments

Researchers analyze seafloor sediment cores to understand past behavior of the Black Current
Posted inResearch Spotlights

Sediment Cores Reveal Ocean Current’s Past Life

by S. Witman 28 July 20179 May 2023

East Asia’s Black Current may have rerouted in the past 10,000 years or so.

For 17,000 years, rain has washed sediments down the slopes of New Zealand’s Southern Alps, depositing them in Lake Ohau.
Posted inScience Updates

Shifting Winds Write Their History on a New Zealand Lake Bed

by G. B. Dunbar, M. J. Vandergoes and R. H. Levy 16 May 201715 February 2023

A team of scientists finds a year-by-year record of climate history spanning the past 17,000 years at the bottom of a South Island lake.

Researchers evaluate remagnetization in sedimentary rocks to better understand the Earth’s tectonic history.
Posted inResearch Spotlights

Diagnosing Cryptic Remagnetization in Sedimentary Rocks

by Terri Cook 9 May 201727 January 2023

To understand the ancient movement of Earth’s tectonic plates, comprehensive magnetic and petrographic studies are needed to detect secondary magnetization in carbonates and other sedimentary rocks.

Researchers assess whether methods of studying alluvial rivers are helpful to understanding behavior of rivers without loose sediment.
Posted inResearch Spotlights

How Do Rivers Flow over Bedrock?

by Terri Cook 8 May 201713 October 2022

A study questions whether the hydraulics of rivers that lack loose sediments along their bottoms can be accurately depicted by standard equations for flow over sediment.

Photomicrogram of sediment coarse fraction from Heinrich Event 1, including forams and grains transported by icebergs.
Posted inResearch Spotlights

Iceberg Surge During Last Deglaciation May Have Had Two Pulses

Sarah Stanley, Science Writer by Sarah Stanley 27 April 20174 May 2022

Seafloor sediment cores provide new clues that could help clarify the influence of ice sheet collapse on a period of ocean cooling marked by slowed deepwater circulation.

As the wind blows across the drylands of Namibia, sand clusters around isolated plants.
Posted inResearch Spotlights

New Tool for Understanding Landscape Evolution in Drylands

by Jenny Lunn 26 April 20172 March 2023

Combining vegetation distribution models and sediment transport models offers a better understanding of how dryland environments change in response to different factors.

A new study uncovers the influence of sediments from high-discharge events on the transfer of momentum between water layers in the Guadalquivir River Estuary.
Posted inResearch Spotlights

Dam Discharge Events Alter Water Flow in an Estuary in Spain

Sarah Stanley, Science Writer by Sarah Stanley 24 April 20171 February 2023

Three-year observations suggest that increased sediment concentrations inhibit vertical transfer of momentum between water layers for more than 2 months after a high-discharge event.

Researchers look at offshore sediments to trace the history of the world’s tallest coastal mountain range
Posted inResearch Spotlights

A Mountain Range's History Preserved in Ocean Sediments

by Terri Cook 7 April 201729 June 2022

Fission track dating core samples from the Gulf of Alaska demonstrates that offshore sediments can be used to reconstruct a mountain range's changing exhumation patterns.

Researchers trace boron in fluids released by subducting slabs to assess how tectonic plates and ocean waters interact at subduction zones.
Posted inResearch Spotlights

Fingerprinting the Source of Fore-Arc Fluids

by Terri Cook 9 February 20178 February 2023

A new model tracks boron and other tracers in fluids expelled from subducting slabs to help identify the fluids' source regions and migration routes.

Antarctic research team scrapes sediment cores from 1200 meters below the seafloor near the Cosgrove Ice Shelf.
Posted inNews

Déjà Vu? Ocean Warmth Melted Ancient West Antarctic Ice Shelf

Sarah Derouin, Science Writer by Sarah Derouin 30 January 201713 December 2021

Clues in seafloor sediments reveal that relatively warm water beneath western Antarctic ice shelves, a major factor in today's massive ice sheet retreat, also fueled some past ice loss.

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