Danielle Meitiv's Barefoot Blog

Writing and life… without shoes


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Where the rare is common and extreme is the norm

The U.S. Census was not the only enumeration completed this year. The Census of Marine Life, an unprecedented collaboration of 2,700 scientists from 81 countries culminated in 2010 after ten years, and more than 540 ocean expeditions. And the results are staggering. The Census documented a changing ocean, richer in diversity, more connected through distribution and movement, more impacted by humans, and yet less understood than previously believed.

Researchers asked three basic questions: What lives is the global ocean?, Where do they live?, and How Many are there?

More than 6,000 new species were discovered, and the estimate of known species increased from 230,000 to 250,000, as genetic analysis revealed that organisms thought to be related were in fact different species. Extrapolating from that, scientists estimate that the total number of marine species is close to one million – meaning that another 750,000 have yet to be found.

Life was found everywhere researchers looked, from temperatures high enough to melt lead to those low enough to freeze seawater, and in places where oxygen was absent. Although the ocean may look uniform from above, these habitat extremes were the norm rather than the exception. Migratory routes and feeding and breeding areas were mapped, showing how interconnected the ocean basins are. Scientists explored parts of the deep sea and sea floor never before seen by human eyes, and found life thriving on ocean ridges, seamounts, abyssal plains, continental margins, and hydrothermal vents.

This Hydrothermal vent snail, Alviniconcha sp. from the Suiyo Seamount, Tokyo Hydrothermal Vent is the only specimen ever found. Photo Credit: Yoshihiro FUJIWARA/JAMSTEC

While the number of species is high, the abundance and size of many of them are decreasing. From the plankton at the base of the food chain to the predators at the top, species are in decline. Since the 1950s, phytoplankton abundance has decreased by 40%. Overfishing and habitat destruction are the leading direct threats to marine life.

Census researchers also discovered things about humans, dividing the causes separating the known from the unknown and the unknowable into five categories:

  1. the invisibility of the parts of the past that have been lost;
  2. the vast expanse of the ocean;
  3. the challenges in assembling knowledge of parts into an understanding of the whole;
  4. events and disturbances that we can’t predict, such as tsunamis, and
  5. the blinders we put on ourselves by choosing not the look or spend the time or money to know.

I have just started to plumb the depths of the papers, presentations, briefings, photos, and maps produced by this unprecedented scientific collaboration. Over the next few months, I will feature a number of posts highlighting the most exciting Census discoveries. In the meantime, I urge you to check out the fabulous resources available for free on their website. Some personal favorites are (so far):

Stay tuned for more on the incredible What, Where, and How Many of life in the global ocean.


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Global Warming Warps Marine Food Webs

(I’m working hard on my fiction writing so I’m taking a bit of a break from the blog. Just another few days and then I’ll be back with more original content, promise! For now, here’s an interesting story reposted from ScienceNOW Daily News)

By Erik Stokstad
ScienceNOW Daily News
26 August 2009

Teasing apart the complex ways in which global warming will affect ocean life has been tough. But new research suggests that a simple ecological theory may explain at least one piece of the puzzle: the effect on marine food webs. And the news may not be all bad.

New experiments confirm that phytoplankton, which form a bottom rung of oceanic food chains, will become less productive in warmer, nutrient-rich water. However, the results also show that zooplankton should boom in these warmer areas, which could benefit certain fisheries.

The food-web theory hinges on the assumption that temperature affects the metabolism of organisms that rely on other creatures for food, like zooplankton, while not having much of an impact on photosynthetic organisms like phytoplankton. That suggests that in warmer waters, zooplankton should generally grow faster and start reproducing sooner than they do in cooler waters. As zooplankton become more abundant and eat more phytoplankton, the population of phytoplankton should shrink.

Mary O’Connor, now a postdoc at the National Center for Ecological Analysis and Synthesis in Santa Barbara, California, and her colleagues set up an experiment to test the theory. They put zooplankton and phytoplankton into 4-liter tubs and let them sit for 8 days. Some were kept at the ambient temperature; others were heated by 2°, 4°, or 6°C. Recognizing that nutrient levels vary in the ocean, they added extra nitrogen and phosphorous to half the tubs in each group.

As temperatures rose, the productivity of the communities without extra nutrients hardly changed. Nor did the food web. This suggests to O’Connor and her colleagues that nutrient-poor food webs may be relatively resilient to global warming. The tubs that got additional nutrients were another story: The zooplankton in warmer water became more abundant while the numbers of phytoplankton fell. In fact, the ratio of zooplankton to phytoplankton rose 10-fold, the team reports in a paper posted online on 25 August in PloS Biology. “It matched our predictions really well,” O’Connor says. She adds that even though overall biological productivity declined as temperature rose, the increase in zooplankton could benefit fish that eat them in nutrient-rich waters.

Ulrich Sommer, a plankton ecologist at the Leibniz-Institut für Meereswissenschaften in Kiel, Germany, calls the shift in the food web “quite dramatic.” (The new findings match those from a similar experiment in which Sommer and colleagues varied light levels rather than nutrients.)

Sommer notes that fish eat only certain kinds of zooplankton, so more analysis is needed to gauge the impact on the food supply. And physical differences between regions, such as currents and the stratification of the water column, will also complicate the response of food webs.

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