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Garbage Vortex Revisited

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On 27 May 2009 I featured the Pacific Garbage Patch. In an article titled “Project Kaisei: voyage to clean up the plastic vortex” CNN has brought some pictures and a video from an August 2009 voyage to the area.

Apart from the CNN text, I think their dreadful images talk for themselves. The most heavily polluted areas of surface water in the gyre contained six times more plastic than plankton biomass.

A further voyage next year hopes to gather more data and move closer to a practical solution to the ever increasing problem.



PS.
More footage from the Kasei project:

Hat tip “Living the Scientific Life” Blog
http://scienceblogs.com/grrlscientist/2009/10/project_kaisei_2009_intro_from.php

See also: http://scienceblogs.com/grrlscientist/2009/10/project_kaisei_scripps_oceanog.php



Academics

Alps Growing or Shrinking?

A couple of months ago I wrote about a new hypothesis by Egholm et al. according to which the maximal mountain height correlate closely with climate-controlled gradients in snowline altitude rather than with tectonic activity. In Denmark this hypothesis seems to have lead to a heavy discussion about the uplift/erosion history of the Norwegian mountains between geologists at the University of Århus versus geologists at the University of Copenhagen, and I am looking forward to hear more about this dispute at the Nordic Geological Winter Meeting in Oslo in January.



But how about the Alps? A paper in the latest volume of the science magazine "Tectonophysics" (No. 474, S.236-249) seems now to prove that today's uplifting of the Alps is driven by strong climatic variations. The formation of the Alps through the collision of the two continents Africa and Europe began about 55 million years ago. By now the Alps are shrinking just as quickly in height, as they are growing. Due to the erosional work of glaciers and rivers about exactly the same amount of material is eroded from the Alps as added by uplifting.

Swiss geodesists, who have been measuring the Alps with highest accuracy for decades, have observed, that the Alp summits, as compared to low land, rise up to one millimetre per year. Over millions of years a considerable height would have to result. Researchers from the GFZ German Research Centre for Geosciences have calculated that the mountains eroded concurrently at almost exactly the same speed.

Though the Alps are constantly rising, it is no longer the plate forces but the strong climatic variations since the beginning of the so-called quaternary glacial before approximately 2.5 million years, to which mountain slopes in particular have been reacting so sensitively. To-days rise is attributed to the melting of Alpine glaciers.

Well, today it is probably just a question of isostasy, i.e. gravitational equilibrium between the earth's lithosphere and asthenosphere, meaning that the Alps "float" at an elevation which depends on their thickness and density. The burning question is, why the Alps stopped “growing”, where they did, during their collision phase. Was this only a question of isostasy or was the “snowline effect” at work?





Academics

Largest Alpine Karst Area In Scandinavia

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The Norwegian Glomfjellet hosts the largest alpine karst area in Scandinavia. The Glomfjell karst consists of some 200 km² metacarbonates containing bands of relatively pure calcite marble (’grey marble’) interbedded with mica schist and less purer, micaeous marble (’yellow marble’).

The karst topography includes caves, dolines, bogazes, and karren.

It is planned to be a “Verneområde” (Area of Conservation) and is in this context described in an article at the Norwegian Geoportalen. Now, although the article is written in Norwegian it contains some really nice pictures of karst and other geologic features in the area for everybody to enjoy - just scroll downwards. So DO click here.

Latitude and longitude 66° 47' 8.95" N 14° 12' 8.04" E

Note:
A bogaz is a type of formation in which the rock (usually limestone) was eaten away along a joint to form a long, narrow cleft or ravine. They often have steep, almost vertical sides. This is exactly the same thing as a grike, except bigger. Boğaz is Turkish for throat.
Karren are furrows or channels formed on the surface of soluble bedrock by dissolution of a portion of the rock. (Also known as lapies.)

In Norwegian:




Academics

Franz Josef Land (in the Arctic)

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Few people know where Franz Josef Land is, or have ever heard of it. Except for a few Russian army border guards, Franz Josef Land is totally uninhabited. It has no native inhabitants. This is not because the area is small - Its 191 islands have a total area of 16,134 km². It is however situated far up north in the Arctic - and was furthermore completely closed to visitors for roughly 60 years until 1991. It is the most northerly group of islands associated with Eurasia and the Eurasian continental plate. Gakkel Ridge further north is normally seen as on the border zone between The Eurasian and the North American plate.

The situation may change now that the sea ice in the Arctic is melting and icebreakers in a few years perhaps no longer may be needed to reach the islands (Most of the Russian icebreakers in the area are - as far as I know - nuclear icebreakers). Since 2005 cruises are organised from Murmansk.

The archipelago is dominated by Jurassic to Tertiary basalts, but there are also late Triassic and Jurassic sediments lying in near horizontal strata. Fossil tree trunks show that the climate here was warmer in the Mesozoic. The basalt layer above the Jurassic sediments is up to 500 m thick and part of a Large Igneous Province (LIP) formed in the Cretaceous, and called the High Arctic Large Igneous Province (HALIP). This is a major Late Cretaceous large igneous province located in the Arctic. It includes the Ellesmere Island Volcanics, Strand Fiord Formation, Alpha Ridge, Franz Josef Land and Svalbard. These areas were closer to each other in the Cretaceous - since then the spreading ridge (Gakkel Ridge) has brought them further apart. A multitude of tectonic fault lines has broken the archipelago into many relatively small islands.

The age of the HALIP volcanic rocks is rather uncertain, but a long period of magmatism between ca. 136 and 80 million years ago has been suggested for the whole LIP.

From 15 June 2009 the archipelago became part of the newly established Russkaya Arktika National Park.







Academics

Tweetday

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Seen on Twitter:
Should you be tweeting (should scientists be tweeting): http://www.cell.com/fulltext/S0092-8674%2809%2901305-1
How Twitter lists work (getting the most of twitter lists) http://dopodomani.me/2009/10/30/twitter-lists/

My tweeted links:
Cambrian Explosion: This Time Its The Calcium That Did It http://bit.ly/2Ly8v4
Ask Dr. Boris Behncke your Etna questions at the "Eruptions" blog http://bit.ly/1qJydQ via @AddToAny
I wonder where? (Unknown Volcanic Eruption) http://bit.ly/4uarDs (Volcanismblog) & http://bit.ly/3L4LRb

Love Links:
Accretionary Wedge # 21 Earth Science Outreach at Magma Cum Laude http://magmacumlaude.blogspot.com/2009/10/accretionary-wedge-21-earth-science.html



Academics

Too much rain, too soon, in Somalia

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Previously, the area around El-Waq had been suffering from drought. Flash floods caused by four days of torrential rains have now displaced more than 15,000 people in the south-western Somalian town of El-Waq near the Kenyan border and submerged most homes and businesses. A lot of livestock (weakened by the drought) have died due to the ongoing rains. El-Waq, like the rest of Somalia, was waiting for the rain but it was too much in too short a time.





Academics

Post Number 700

I see that I have reached post number 700 today - and there is still so much more to write about. Unbelievable in fact. You are not rid of me yet.

Thanks to all my readers that keep coming. This month the counter has passed 8000 unique visitors this month alone (most of them to visit some of the 699 older posts to be sure).

A special thanks to those that have followed me more or less regularly for the last four years (or less), and to subscribers by email and news feeders. And of course the kind people that link to my blog, without your support I would be nowhere.

Thank you all !



Academics

Dinosaurs died out, but what about Insects?

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The Cretaceous–Paleogene extinction event, which occurred approximately 65 million years ago, was a large-scale mass extinction of animal and plant species in a geologically short period of time. The most famous victims were the dinosaurs. More than half of the species that lived in the sea died out at this time - including ammonites and rudists.

What happened to the insects?

Gunnar Ries at Amphibol commented in a post of 28 October 2009 some of the different causes used to explain the extinction event. His post is in German. This post drew my attention (thank you!) to a publication by a team of biologists form Bonn in the Proceedings of the Royal Society.

Previous studies of insect-damaged fossil leaves in the US Western Interior showed major plant and insect herbivore (plant feeding) extinction at the Cretaceous–Palaeogene boundary. The Bonn team studied leaf fossils from the middle Palaeocene Menat site, France, which has the oldest well-preserved leaf assemblage from the Palaeocene of Europe, to test the generality of the observed Palaeocene US pattern. Apparently the insects were harder hit in the US than in Europe, and where it took about 10 million years for the insect fauna in the US to recover, Europe did in half that time, namely only 5 million years.

The diversity and complexity of plant–insect interactions at Menat suggest that the net effects of the Cretaceous–Paleogene extinction were less at this greater distance from the Chicxulub, Mexico, impact site. Along with the available data from other regions, the study seems to show that the end-of-Cretaceous event did not cause a uniform, long-lasting depression of global terrestrial ecosystems. Rather, it gave rise to varying regional patterns of ecological collapse and recovery that appear to have been strongly influenced by distance from the Chicxulub structure.

This does not end the discussion, but seems to back up the Chicxulub hypothesis. Who makes the next goal?

Reference:
Wappler et al.
No post-Cretaceous ecosystem depression in European forests? Rich insect-feeding damage on diverse middle Palaeocene plants, Menat, France
Published online before print September 23, 2009
doi: 10.1098/rspb.2009.1255

Unfortunately NOT open access !

The Palaeocene Epoch is a geologic epoch that lasted from around 65 to around 56 million years ago.
The Palaeogene Period (that began around 65 and ended around 23 million years ago) on the other hand comprises the Palaeocene, Eocene and Oligocene





Academics

Open Access is Good Business

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Hereby a few quotes from a press release from Denmark’s Electronic Research Library.

“Denmark could make millions if researchers at universities and educational institutions made their reports freely available online.”

“Currently, most research results are published in scientific journals run by commercial publishers, but the results would reach a much broader audience if access were free. This would make research act as a knowledge dynamo, supporting the further development within the segment of small businesses. The study shows that open access to research would yield societal benefits worth DKK 300 million annually (approx. EUR 40 million).”

“It’s common sense to make publicly funded research freely available online so we can all benefit from it ... Currently, you have to pay to gain access to the newest knowledge in research, and that’s why we don’t benefit from the large public investments in research. Knowledge and innovation are Denmark’s most important raw materials and open access to research results will contribute to a larger dissemination and therefore a better utilisation of those raw materials.”

“Denmark is among the countries who have committed to the promotion of the EU policy of free online access to research results.”







Academics

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