Mostrando entradas con la etiqueta Salt marsh. Mostrar todas las entradas
Mostrando entradas con la etiqueta Salt marsh. Mostrar todas las entradas

sábado, 1 de octubre de 2016

the National Science Foundation (NSF) : Discovery Changing salt marsh conditions send resident microbes into dormancy.- Condiciones cambiantes en el pantano de sal, envían microbios residentes en lactancia..............

https://www.nsf.gov/discoveries/disc_summ.jsp?cntn_id=189412&WT.mc_id=USNSF_57&WT.mc_ev=click
Over time, nutrients such as nitrogen affect important marsh bacteria
Sunset over a salt marsh at Plum Island, Massachusetts, as autumn arrives.

Sunset over a salt marsh at Plum Island, Massachusetts, as autumn arrives.
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September 26, 2016
The following is part 22 in a series on the National Science Foundation's Long-Term Ecological Research (LTER) Network. Visit parts one, two, three, four, five, six, seven, eight, nine, 10, 11, 12, 13, 14, 15, 16,17, 18, 19, 20 and 21.
Could the future of a salt marsh be hidden in the health of its microbes? Scientists say yes.
Salt marshes play key roles in reducing the effects of urbanization and climate change. Marshes absorb carbon dioxide from the atmosphere, and their microbes break down carbon.
That's why researchers are working to find out how these vital ecosystems tick.
Jennifer Bowen of Northeastern University and colleagues have studied microbes in the sediments of salt marshes in the National Science Foundation (NSF) Plum Island Ecosystems Long-Term Ecological Research (LTER) site in northeastern Massachusetts.
They're working to discover how the marsh -- and the microbes in it -- change over time when outside influences, such as nitrogen, are introduced to the ecosystem.
"A lot of the ecological services salt marshes provide are facilitated by microbes," Bowen said. "They're involved in the carbon cycle and the nitrogen cycle, and they remove nutrient pollution through their metabolic processes."

Dormant microbes

In a new paper published in the journal Nature Communications, Bowen and her Northeastern colleague Patrick Kearns, who is first author of the paper, along with researchers at the Marine Biological Laboratory and Woods Hole Oceanographic Institution, set out to discover what would happen to microbes in salt marshes if specific nutrients were added to the environment -- through urbanization and climate change, for example.
Adding nutrients like nitrogen produced no change in the types of bacteria present in the salt marsh -- at least, temporarily. But over time, a large number of the microbes became dormant.
"It's kind of like a bear going into hibernation," Bowen said. "These dormant bacteria are in a low metabolic state. They just bide their time until environmental conditions return that are suitable for them."
When the microbes go dormant, they don't contribute to the critical ecosystem services that make salt marshes important.

Human-salt marsh interactions

"This study shows that human activities are affecting bacteria essential to salt marshes in ways we never suspected," said Matt Kane, program director in the NSF Division of Environmental Biology, which co-funded the research with NSF's Division of Ocean Sciences. "Coastal salt marshes provide many benefits -- supporting diverse wildlife, helping to reduce pollution, and protecting us from flooding."
What happens to salt marshes and their bacteria, Kane explained, ripples into human lives.
The study's results help explain why salt marshes contain so much microbial diversity. One group of microbes is specialized for a specific set of conditions, while another is linked with others. As the environment changes, different bacteria take advantage of the conditions that are most suitable to them.
"These investigators have made an important discovery about the resilience of microbial communities in salt marsh ecosystems," said David Garrison, program officer in NSF's Ocean Sciences Division.
A salt marsh, the researchers say, is a constant balancing act.
"If we see an increase in the abundance of bacteria that are able to decompose the marsh, we also see an increase in bacteria that can help fix carbon," Bowen said. "If a marsh is failing, there is no way to restore the microbes. But what can be created is an environment that will help these microbes thrive."
To save the marshes, she said, save their microbes.
-- Cheryl Dybas, NSF (703) 292-7734
  cdybas@nsf.gov
-- Lori Lennon, Northeastern University (617) 373-7686
  l.lennon@northeastern.edu


Investigators Jennifer Bowen
Related Institutions/Organizations University of Massachusetts Boston
Related Awards #1353140 Collaborative Research: Ecosystem Evolution and Sustainability of Nutrient Enriched Coastal Saltmarshes
Total Grants $220,177
Related WebsitesNSF Plum Island Ecosystems LTER Site:
https://lternet.edu/sites/pie
NSF Long-Term Ecological Research discovery articles series: https://www.nsf.gov/discoveries/disc_summ.jsp?cntn_id=138170
The Plum Island marsh expanse in summer at low tide.
The Plum Island marsh expanse in summer at low tide.
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Researcher Patrick Kearns fills tubes of mud to look at microbes' responses to nutrients.
Researcher Patrick Kearns fills tubes of mud to look at microbes' responses to nutrients.
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Low tide in the marsh, with
Low tide in the marsh, with "Frank the Tank," a nutrient delivery system, in the background.
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Patrick Kearns samples salt marsh sediments from West Creek on Plum Island.
Patrick Kearns samples salt marsh sediments from West Creek on Plum Island.
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Researchers take a break from field sampling in Plum Island's salt marshes.
Researchers take a break from field sampling in Plum Island's salt marshes.
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the National Science Foundation (NSF)
Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com
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domingo, 13 de abril de 2014

ESA : Salt marsh, Kazakhstan


This satellite image was acquired over the edge of a salt marsh near the northeast Caspian Sea in southwestern Kazakhstan.
The Caspian Sea (not pictured) is the largest inland body of water by surface area. With an average depth of about 5 m, the northern part of the Caspian is very shallow, while the central and southern parts of the sea are much deeper. The salinity of the waters also change from north to south, being more saline in the northern, shallow waters and and less in the south.
The salt marsh in the upper section of this image was once a gulf of the Caspian Sea, but fluctuating sea levels over the last decades cause it to be cut off occasionally from the main body of water and even dry up. In this image, it appears that the water has evaporated, leaving behind a white salt crust.
Rock formations dominate the central part of the image, while a plateau stretches south and east (not pictured). The visible shapes in combination with the dark colour of the rocks may indicate that they are volcanic, with water erosion evident in the finger-like runoff patterns.
The grey rim between the land and salt pan comes from the sedimentary runoff from the land mixing with the saltwater. When the marsh is dry, a greyish colour is left behind.
The arid climate in this region makes it easy to acquire optical imagery from satellites, without the obstruction of visibility by clouds.
This image was acquired on 6 November 2012 by the Korea Aerospace Research Institute’s Kompsat-2 satellite and is featured on the Earth from Space video programme.
ESA
Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com
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