Saturday, September 29, 2012

Osteoporosis??


When most people think of sponges, they think of the synthetic sponges that one might buy in a supermarket.       I usually think of natural sponges.  Natural sponges are a group of some of the simplest "complex" animals on the planet.  Their simplicity certainly does not suggest any predation.

Below is an interesting article on how certain types of sponges are seriously impacting some coral reefs.

Osteoporosis in the World's Oceans: Bioeroding Sponges Are Threatening Coral Reefs

ScienceDaily (Sep. 19, 2012) — Due to the massive production of the greenhouse gas carbon dioxide, our oceans are becoming increasingly acidic. Scientists of Senckenberg am Meer in Wilhelmshaven studied the consequences of ocean acidification on sponges that bore into calcareous materials such as coral skeletons. Results show that these sponges will profit from global changes, while coral reefs are threatened in their survival.
The study was published in the online journal PLoS ONE.
Increasing concentrations of carbon dioxide are not only changing the atmosphere, but also the oceans: Carbon dioxide reacts with water and forms carbonic acid, which acidifies the seas. The pH decreases simultaneously with this acidification, having mostly negative effects on many organisms in our oceans.
"Especially organisms that form calcareous skeletons, such as corals, will have to expend more energy in more acidic conditions," states Dr. Max Wisshak from Senckenberg am Meer in Wilhelmshaven. "In contrast -- so our hypothesis -- organisms that bioerode calcareous skeletons by biochemical etching should have an easier job in future and should thus be counted into the small circle of winners of the global change."
To test this hypothesis the team of scientists in collaboration with the Australian Institute of Marine Science and GEOMAR -- Helmholtz Centre for Oceanography in Kiel conducted elaborate experiments at the largest coral reef on earth, the Australian Great Barrier Reef, working with the bioeroding sponge Cliona orientalis. This demosponge is widely distributed, belongs to the most aggressive bioeroders, and will in future very likely contribute even more to the erosion of many coral skeletons in the Great Barrier Reef.
"We were able to confirm a clear relationship between the pH of the seawater and the bioerosion rate of these sponges," says Wisshak. "Our data predict an up to 25 percent increase of sponge bioerosion until end of this century!"
As bioeroding sponges often contribute the lion share of coral bioerosion on tropical reefs, with increasing ocean acidification the reefs will be exposed to a duplicate burden: calcification will be more difficult, and existing skeletons will be more strongly weakened by bioerosion. "This may lead to a shift from present-day positive reef growth to future negative budgets with stronger reef bioerosion. In consequence our reefs would be threatened by yet another stress factor," explains the marine geologist from Wilhelmshaven.
Testing effects of rising sea surface temperatures in the world's oceans -- another consequence of the present global change -- revealed a comparatively small influence on bioerosion rates of the sponges. What the sponges do not mind has a serious outcome for corals: Rising temperatures have a large impact on corals: Heat stress causes "bleaching" in corals, and in consequence they can die in dramatic mass mortality events.
The outcome of severe bleaching events is disastrous as reefs are home to many marine organisms and the basis of a complex food chain -- all the way up to humans.
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The above story is reprinted from materials provided bySenckenberg Research Institute and Natural History Museum.
Note: Materials may be edited for content and length. For further information, please contact the source cited above.

Journal Reference:
  1. Max Wisshak, Christine H. L. Schönberg, Armin Form, AndrĂ© Freiwald. Ocean Acidification Accelerates Reef BioerosionPLoS ONE, 2012; 7 (9): e45124 DOI:10.1371/journal.pone.0045124
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Senckenberg Research Institute and Natural History Museum (2012, September 19). Osteoporosis in the world's oceans: Bioeroding sponges are threatening coral reefs.ScienceDaily. Retrieved September 29, 2012, from http://www.sciencedaily.com­/releases/2012/09/120919082924.htm
Note: If no author is given, the source is cited instead.
Disclaimer: Views expressed in this article do not necessarily reflect those of ScienceDaily or its staff.
Ocean Acidification In The Caribbean Significant, Yet Variable (Nov. 28, 2008) — A new study, which confirms significant ocean acidification across much of the Caribbean and Gulf of Mexico, reports strong natural variations in ocean chemistry in some parts of the Caribbean that ...  > read more

Wednesday, September 19, 2012

Where Has All The Ice Gone?

I used this same post for the Earth Science blog.  Sea ice coverage is certainly important for oceanography.



During the current melting season, sea ice coverage on the Arctic Ocean reached its all-time recorded low.  This year's low measured even less than the previous record, 2007.

Although many still energetically debate the causes, they cannot ignore the Arctic warmup of the past 10 or so years.

The lower ice coverage will affect marine life (including polar bears - officially a marine mammal) and will further contribute to Arctic warming.

Scientists do not know the cause(s) nor do they know what future changes are in store.

Below is a phenomenal NOAA animation of satellite still images illustrating this year's loss of ice.


Sunday, September 16, 2012

The Last Frontier

Mission Plan: Proposed remotely operated vehicle dive sites at major features of interest in the Northeast Lau Basin
Some scientists speculate that we know more about space, our solar system, and the universe, than we do about the largest general environment on our planet - the world ocean.

There has been a lot of interest in ocean exploration the past few years - James Cameron, Bob Ballard, etc.

NOAA is helping lead an expedition looking at backarc volcanoes in the western Pacific Ocean and the organisms found there.

Click this link to the NOAA Ocean Explorer: NOAA Ocean Explorer

Saturday, September 15, 2012

Salinity

Given our current discussions regarding seawater chemistry, I thought the following article from Woods Hole Oceanographic Institution was timely.


NASA/WHOI Voyage Set to Explore Link Between Sea Saltiness and Climate

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A NASA-sponsored expedition is set to sail to the North Atlantic's saltiest spot to get a detailed, 3-D picture of how salt content fluctuates in the ocean's upper layers and how these variations are related to shifts in rainfall patterns around the planet.
The research voyage is part of a multi-year mission, dubbed the Salinity Processes in the Upper Ocean Regional Study (SPURS), which will deploy multiple instruments in different regions of the ocean. The new data also will help calibrate the salinity measurements NASA's Aquarius instrument has been collecting from space since August 2011.
SPURS scientists aboard the research vessel Knorr leave Sept. 6 from the Woods Hole Oceanographic Institution in Woods Hole, Mass., and head toward a spot known as the Atlantic surface salinity maximum, located halfway between the Bahamas and the western coast of North Africa. The expedition also is supported by the National Oceanic and Atmospheric Administration and the National Science Foundation.
The researchers will spend about three weeks on site deploying instruments and taking salinity, temperature and other measurements, before sailing to the Azores to complete the voyage on Oct. 9.
They will return with new data to aid in understanding one of the most worrisome effects of climate change -- the acceleration of Earth's water cycle. As global temperatures go up, evaporation increases, altering the frequency, strength, and distribution of rainfall around the planet, with far-reaching implications for life on Earth.
"What if the drought in the U.S. Midwest became permanent? To understand whether that could happen we must understand the water cycle and how it will change as the climate continues to warm," said Raymond Schmitt, a physical oceanographer at Woods Hole and principal investigator for SPURS. "Getting that right is going to involve understanding the ocean, because the ocean is the source of most of the water."
Oceanographers believe the ocean retains a better record of changes in precipitation than land, and translates these changes into variations in the salt concentration of its surface waters. Scientists studying the salinity records of the past 50 years say they already see the footprint of an increase in the speed of the water cycle. The places in the ocean where evaporation has increased and rain has become scarcer have turned saltier over time, while the spots that now receive more rain have become fresher. This acceleration ultimately may exacerbate droughts and floods around the planet. Some climate models, however, predict less dramatic changes in the global water cycle.
"With SPURS we hope to find out why these climate models do not track our observations of changing salinities," said Eric Lindstrom, physical oceanography program scientist at NASA Headquarters in Washington. "We will investigate to what extent the observed salinity trends are a signature of a change in evaporation and precipitation over the ocean versus the ocean's own processes, such as the mixing of salty surface waters with deeper and fresher waters or the sideways transport of salt."
To learn more about what drives salinity, the SPURS researchers will deploy an array of instruments and platforms, including autonomous gliders, sensor-laden buoys and unmanned underwater vehicles. Some will be collected before the research vessel heads to the Azores, but others will remain in place for a year or more, providing scientists with data on seasonal variations of salinity.
Some of the devices used during SPURS to explore the Atlantic's saltiest spot will focus on the outer edges of the study area, traveling for hundreds of miles and studying the broadest salinity features. Other instruments will explore smaller areas nested inside the research site, focusing on smaller fluxes of salt in the waters. The suite of ocean instruments will complement data from NASA's salinity-sensing instrument aboard the Aquarius/SAC-D (Satelite de Aplicaciones Cientificas-D) observatory, and be integrated into real-time computer models that will help guide researchers to the most interesting phenomena in the cruise area.
"We'll be able to look at lots of different scales of salinity variability in the ocean, some of which can be seen from space, from a sensor like Aquarius," said David Fratantoni, a physical oceanographer with Woods Hole and a member of the SPURS expedition. "But we're also trying to see variations in the ocean that can't be resolved by current satellite technology."
The 2012 SPURS measurements in the North Atlantic will help scientists understand the behavior of other high-salinity regions around the world. A second SPURS expedition in 2015 will investigate low-salinity regions where there is a high input of fresh water, such as the mouth of a large river or the rainy belts near the equator.

The Woods Hole Oceanographic Institution is a private, non-profit organization on Cape Cod, Mass., dedicated to marine research, engineering, and higher education. Established in 1930 on a recommendation from the National Academy of Sciences, its primary mission is to understand the oceans and their interaction with the Earth as a whole, and to communicate a basic understanding of the oceans' role in the changing global environment.
Originally published: September 5, 2012

Monday, September 3, 2012

Arctic Sea Ice


The Arctic Ocean's cloak of pack ice has thinned and shrunken during the past 30 years.  However, the Arctic has warmed more than any other part of the globe during that same time frame.  The exact reason still elude scientists.

This summer the Arctic Ocean reached a new milestone.  Read on to find out which one...


As of August 26, Arctic sea ice appears to have broken the 2007 record for smallest daily extent of the satellite era. Arctic sea ice extent fell to 1.58 million square miles on August 26, 2012. This was 27,000 square miles (slightly bigger than the state of West Virginia) below the previous record low of 1.61 million square miles, set in September 2007.
Map of the arctic showing the previous sea ice extent record low in 2007
The official 2012 minimum extent can’t be declared until scientists are sure the summer melt season is over, but the final figure will likely be still lower: there are two to three more weeks left in the melt season, and sea ice continues to track below 2007 daily extents. In the first half of August, ice was melting at a rate of just over 43,000 square miles per day. The pace of ice melt in late August 2012 had slowed to about 29,000 square miles per day, but that was still nearly double the normal rate for this time of year.
Arctic sea ice extent (areas with 15% or more ice cover) on August 26, 2012, based onsatellite data from the National Snow and Ice Data Center. Orange line shows the boundary of the previous record low sea ice extent. (Map by climate.gov team.)
graph of previous arctic sea ice extent record low in 2007 and the new lower record in August 2012
Graph of five-day-mean sea ice extents in the Arctic over the course of the year. On August 26, ice extents fell below the previous record low observed by satellites in September 2007. Graph courtesy National Snow and Ice Data Center’s Arctic Sea Ice News & Analysispage.
In a media advisory issued by the National Snow and Ice Data Center, NSIDC scientist Walt Meier said of the new record low, “By itself it’s just a number, and occasionally records are going to get set. But in the context of what’s happened in the last several years and throughout the satellite record, it’s an indication that the Arctic sea ice cover is fundamentally changing.”
Among the many signs of fundamental change is that ice thickness is declining as fast or faster than area. The Arctic was previously dominated by ice that had survived multiple summer thaws, growing steadily thicker over the years. Today, very little of this old, thick ice remains.
Reviewed by Ted Scambos, National Snow and Ice Data Center.