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How genetic islands form among marine molluscs

A new study explains how genetic islands can occur in marine molluscs by studying the limpet Nacella concinna. The researchers found that an entire generation of offspring descended from a limited number of parents and were carried by ocean currents to one location.

SourceBielefeld University·JournalScience Advances·TypeObservational study·DateSep 13, 2021

Thwaites glacier: Significant geothermal heat beneath the ice stream

Researchers have mapped significant geothermal heat beneath Thwaites Glacier in West Antarctica, revealing a new potential weak spot in the ice sheet's stability. This heat flow, estimated to be up to 150 milliwatts per square meter, could lead to easier sliding of the glacier and potentially accelerate its collapse.

Ozone pollution has increased in Antarctica

Researchers analyzed 25 years of Antarctic data, finding that ozone levels near the ground have risen by up to 0.14 ppb per year, primarily driven by natural and human sources. This increase can have negative impacts on the region in the future due to ozone's ability to trap heat near Earth's surface.

SourceAmerican Chemical Society·JournalEnvironmental Science & Technology·DateJun 16, 2021

Māori connections to Antarctica may go as far back as 7th century, new study shows

A new study published in the Journal of the Royal Society of New Zealand suggests that indigenous Māori people may have set eyes on Antarctic waters and possibly the continent as early as the 7th century. The research uncovers a deep-rooted connection between Māori people and Antarctica, which continues to this day.

SourceTaylor & Francis Group·JournalJournal of the Royal Society of New Zealand·DateJun 9, 2021

Pandemic paleo: A wayward skull, at-home fossil analyses, a first for Antarctic amphibians

Researchers at the University of Washington successfully analyzed Micropholis stowi fossils excavated during a 2017-2018 collection trip to Antarctica. The findings reveal that this salamander-sized amphibian was more widespread than previously recognized, with evidence suggesting it could have adapted to various environments.

SourceUniversity of Washington·JournalJournal of Vertebrate Paleontology·DateMay 21, 2021

Earthquake creates ecological opportunity

A University of Otago study found that the 1855 Wairarapa earthquake created an ecological opportunity for a previously South Island restricted seaweed species to colonize and establish itself in the North Island. This discovery highlights the potential of tectonic disturbance to shape biodiversity, including marine environments.

SourceUniversity of Otago·JournalJournal of Phycology·DateMay 19, 2021

Scientists observe rapid ozone fluctuations over the Antarctic polar vortex edge area

A recent study published in Advances in Atmospheric Sciences found that the polar vortex plays a key role in Antarctic stratospheric ozone depletion. The research used ZSL-DOAS techniques to measure ozone depletion near the edge of the polar vortex, revealing a positive correlation between PV and total ozone columns.

SourceHefei Institutes of Physical Science, Chinese Academy of Sciences·JournalAdvances in Atmospheric Sciences·DateMay 11, 2021

Modelling ancient antarctic ice sheets helps us see future of global warming

Researchers at UMass Amherst used a novel approach to model ancient Antarctic ice sheets, revealing a thick but diminished ice sheet under mid-Miocene warmest conditions. The study suggests that greater precipitation led to a thickening of the ice sheet's interior regions, with potential implications for future sea level rise.

SourceUniversity of Massachusetts Amherst·JournalEarth and Planetary Science Letters·DateApr 15, 2021

Rapid ice retreat during last deglaciation parallels current melt rates

A new study shows that rapid ice melt in the Arctic during the last deglaciation parallels current melt rates, raising concerns about climate change. The research used marine sediment cores to reconstruct the state of the environment 20,000-10,000 years ago and found a consistent correlation between global warming and ice sheet retreat.

SourceUiT The Arctic University of Norway·JournalQuaternary Science Advances·DateFeb 10, 2021

Measuring melting ice

University of Delaware Assistant Professor Carlos Moffat studies coastal systems and glacial ice retreat to understand global sea level rise. He will investigate freshwater discharge and its impact on ocean circulation and marine organisms.

Ice sheets on the move: how north and south poles connect

A new study by McGill University researchers demonstrates that changes in the Antarctic ice sheet were driven by melting ice sheets in the Northern Hemisphere. The team used numerical modeling and geological records to simulate simultaneous changes in sea levels and ice dynamics, revealing a complex connection between the two hemispheres.

SourceMcGill University·JournalNature·DateNov 25, 2020

New clues shed light on importance of Earth's ice sheets

Researchers found subglacial waters in Antarctica and Greenland have higher concentrations of essential trace elements, challenging scientists' understanding of the Earth's geochemical processes. These discoveries may significantly impact the development of healthy ecosystems and the ocean waters receiving ice sheet meltwater.

SourceFlorida State University·JournalProceedings of the National Academy of Sciences·DateNov 23, 2020

Ice loss likely to continue in Antarctica

A new international study by Monash University reveals that Antarctica's ice loss is expected to continue unabated for a long time, even if climate change is brought under control. The study found that rapid ice loss rates in the recent geological past were similar to those observed in rapidly changing parts of Antarctica today.

SourceMonash University·JournalGeology·DateOct 21, 2020

Researchers provide most detailed and complete record yet of Earth's last magnetic reversal

A team of researchers in Japan has created the most detailed and complete record yet of Earth's last magnetic reversal. The study reveals that the geomagnetic field became unstable at least 10,000 years prior to the magnetic direction change 773,000 years ago, and the full reversal process took at least 20,000 years.

SourceResearch Organization of Information and Systems·JournalProgress in Earth and Planetary Science·DateOct 21, 2020