text:
Simple Offset Paper Saddle Stitching Binding , Disney Children Books
1. world advanced printing&binding machine
2. Environment-friendly paper&ink
3. Customized size,page
4. short leadtime
5. Competitive price and prompt shipment
6. Good quality control systerm
1. Cover: 200gsm C2S paper,4/4C,with glossy/matt lamination, Matt/gloss varnish, UV coating, hot stamping, silver, hot stamping gold, embrossing…etc
2. Insides: 80gsm~157gsm FSC C2S art paper or 60~120gsm acid-free paper
,4/4C printing,matt/gloss printing varnishing, 16/32/48P,and so on;
3. Binding: Saddle stitching.
4. MOQ:1000pcs.
5. sample lead time:2-7days
6. sample set up charge: free for blank dummy , courier cost collected(if have no order)
7. Quality control(Control by six steps)
First,our professional designers will check customer's files/artworks carefully,and feedback problems to customer within 4 hours.If the files/artworks without problems,we'll output ozalids for checking before output CTP,and if ozalids are OK,then we'll go ahead.
The printing sheets will be spot checked by printing captain and supervisor at any time when in printing.
After printing, the printed sheets will be checked by QC staff piece by piece to make sure the color are same as approval sample
The semi-finished products will be spot checked by QC staff,and checked piece by piece before moving to next step.
At the end of each line, before packing into cartons, products will be checked one by one by QC staff
After production finished, a random test of proportion ranging from 3% to 5% will be conducted
We strictly follow the 6 steps listed above to conduct production on-line checks and final inspection. And all goods will be conducted spot checks before being loaded into container
As a professional printer with about 20 years printing experience, we supply with all kinds of printing service. In book printing range, we always supply high quality hardcover book printing, soft cover book printing with all kinds of surface finish technics.
More specification as below :
professional saddle stitching book printing
Paper material:
Art paper, cardboard paper, fancy paper, speciality paper, offset paper / wood-free paper etc. per your requirements.
Paper weight:
For cover:
200gsm, 250gsm, 300gsm, 350gsm art paper;
For text:
105gsm, 128gsm, 157gsm, 200gsm, 250gsm art paper;
CMYK full color offset printing, panton color printing, black & white printing.
Binding methord:
Saddle stitching,perfect binding, sewn binding, saddle stitched binding, spiral binding or wire-o binding.
Finishing effect:
Gloss or matte lamination, UV Varnish, Aqueous coating, Spot UV, Embossing & debossing, Hot foil stamping, Glittering, Die cutting, etc.
Magnet, ribbon, EVA foam, plastic tray, sponge, PVC/PET/PP window, discs, small toys like crayons, markers, garland paper, watercolors, glues, pen, pencils, and so on.
Artwork format:
PDF, Adobe Illustrator, Photoshop, Indesign files.
Packing details:
Double Wall Corrugated Carton for Exporting and craft paper warpped inside, size per your book specifications.
1000pcs per title.
Competitive Advantage:
1. 100% manufacturer
Guangdong Xinyuan Color Printing Co., Ltd. is a modernized printing company. We are located in the printing site in the south of China---Guangzhou, Guangdong Province, with RMB600 million registered capital and about 1000 million fixed assets. Our company was built in 1996 and our factory buildt and storage warehouse cover an area of about 25,000 square meters.
2. Advanced Equipments
1. Heidelberg five color offset printing machine
2. Heidelberg 2color offset printing machine SORSZ
3. Heidelberg 5 colors offset printing machine HD102F,
4. Weihai Hamada 1 color offset printing,
5. Beiren web printing 2 color 2 sides,
6. Laser Transfer Printing Machine,
7. Muller Matini perfect binding machine,
8. KOLBUS case-in line machine,
9 Automatic EMS envelope machine,
10. Automatic die-cut machine,
11. Komori Lithron four color machine,
12. Roland two color machine ,
13. CTP pre-press system,
Completed range of post-press machines
3. Excellent and Experienced staff
We have an excellent team composed of 150 professionals and more than 400 skilled workers.
4. Certificates
ISO14001:2004 certificate,
ISO9001:2008 Certificate,
Disney authorized certificate
About our company
1. Company history
Founded in 1996,17 years printing history,With professional service
system, good credit and outstanding business achievement, approved
by National Post Office, Keeping the principle of "good quality,
customer focus", based on the leading forecast, high-tech equipment
and advanced technology, well-trained workforce and highly
efficient management, Moreover, we have established good
cooperation with our clients, such as provincial and municipal
governments, Chinese Post Office, Chinese Philately Corporation
Headquarter, publisher groups, various banks, Disney and Baxter
2. Factory visit is welcome
Only one-minute by car to the Round-city Highway, Guangshen Highway and Hanxi Changlong Highway, also very close to Guangzhou Science City.warmly welcome to visit our factory
Simple Offset Paper Saddle Stitching Binding , Disney Children Books Images


text:
Useful targets
From Openembedded.org
Revision as of 06:50, 13 September 2010 by Sledz (talk | contribs) (Undo revision 2589 by 126.96.36.199 (Talk))
Builds a static executable that prints hello world, then loops infinitely.
Build everything. This takes a long time, a lot of network bandwidth, and a lot of disc space. Can also break your toolchain.
Target to update the "feed" files (Package*) to reflect the current set of .ipk's that exist in the deploy directory. Commonly used after building some packages individually to update the feed and allow them to be installed via a package manager or the opkg command line tools.
Builds the appropriate kernel for your device.

subset: commoncrawl


text:
Nā Palapalai's highly anticipated new album, Ha'a!
2012 brings us to our newest release, HA'A. It is a tribute to our fans whom have somehow, Mahalo Ke Akua, become a Hawaiian music army, worldwide. Your unwavering support humbles us every day. We also dedicate this to all the hula dancers around the world, in countries we could have never dreamed of. It is for you that we sing.
We Aloha you all. The shy, keiki hula, the serious competition hula dancers, the ones who kaholo when they clean their hale. It is for you that we sing. If you Kalākaua in the shower, we bid Aloha to you. Mahalo to the Aunties dancing hula in the front row with a beer in one hand and smoke meat in the other. It is for you that we sing. We most humbly offer you, HA'A. Now get up and dance.
–Nā Palapalai 2012


text:
OK...maybe not "fun", but definitely interesting...
What would be the best way to grab a URL from the body of an email, dump it to whois, and then append the results to an email?
I see the biggest challenge as parsing the URL from the body of the email and dumping it to whois. Not only does the script have to find the url (look for "http://" perhaps?), but it has to take everything between http:// and the first slash. Otherwise, the whois tool wouldn't know what to do with a full URL such as http://www.example.com/path/to/something.htm.
The other issue I see is differentiating between HTML and plaintext emails. I guess the script would have to check for HREF tags first and if they exist look for http between the "<a href>" tags.
Also, I think it'd be ideal to only perform one whois per message. If multiple links exist within the body, there'd be a painful amount of whois data appended in the email.
I've been looking at the DNSBL script for insight, but I'm not experienced or talented enough with Pocoscript to figure this out.
Any thoughts on this? Unrealistic?


text:
Eastern Panhandle Events, Coupons, Reviews!
Eastern Panhandle Events, Coupons, Reviews!
I was recently offered tickets to the Medieval Times Dinner Show Buena Park in exchange for a review. I said yes right away beacause we've always wanted to go and I knew my son would love it. All opinions are mine I promise!
My almost tween son loves history. Documentaries, books, toys, you name it he loves it if it's related to history. We homeschool part time but the medieval time period isn't a subject we've covered. He knows enough about how people lived during that time by learning about history on his own. I took along my tween daughter (who is not at all interested in history unless American Girls are involved) and my youngest son.
We live in San Diego and planned to go to a Friday night 6:30 show. We left the house mid afternoon and hours later when the show started we were still stuck in traffic. By the time we arrived there we had missed most of the dinner show. I asked if we could possibly exchange our tickets for the 8:45 showing and the person behind the ticket counter happily agreed to change the time. From there the customer service remained awesome from the time they gave us our crowns to our waiter at dinner. Everyone was kind, in character, and had a great attitude.
When you head into the first "castle" of Medieval Times you're assigned a knight to cheer for during dinner. We were given the red knight and each received a paper crown with the corresponding color. You can get group pictures taken in costume in front of a green screen with a choice of backgrounds or pictures with royalty. Pictures cost $21 and an extra $3 if you want to be in costume. We didn't get pictures taken. The next stop was to buy a flag for the red team. I hadn't planned to buy one, trying to keep cost to a minimum, but for $5 my kids shared a flag and enjoyed waving it any time the red knight competed in the arena.
The main "castle" is huge with several counters to buy souvenirs (we didn't) a couple bar counters, and windows to view into the paddocks. Dinner seating and the arena are through a separate set of doors that remain closed until you're called by team for the show.
While we waited for our dinner there was entertainment with some of the night's royalty being called out. This includes birthdays and other events people are there to celebrate.
The show starts with the announcement of the king and princess. Next horses enter the arena to show off some pretty amazing tricks. Each team is seated in separate sections for dinner so we were surounded by other red knight fans. As far as I could see there wasn't a bad view from any seat in the arena.
The knights come out on their horses and stand near their sections and the kids go crazy cheering. From there the show continues with games, a plot twist, and carnations tossed in the audience by winning knights. The jousting was fun to watch because the knights really got into the games.
Each knight chooses a queen of the tournament from his section of the crowd and my daughter was chosen! It was an exciting and sweet moment that added to our enjoyment of the night. She got a sash to wear and they took her photo. My complaint of the evening is that they tried to charge me $21 for the photo. I didn't buy it.
The tournament ends with a series of sword battles. These battles are really realistic and scared my youngest son enough to have him hiding under the table. Sparks literally fly as the swords clash and it gets pretty intense.
We were greeted by our waiter and given options for drinks. Dinner is served in courses all at once to the whole audience. Our show served garlic bread, tomato bisque, chicken, a baked potato, corn on the cob, and a lemon pastry. A vegetarian option was also available.
I have two things to say about the medeival times food. It was better than I expected and the temperature was perfect. We didn't have to wait for the food to cool down (a huge plus with kids) and everything was delicious. Keep in mind that there are no untensils but I think that adds to the fun!
Dinner ends with coffee and a tip tray. The price of dinner and the show doesn't include a tip so bring cash to give your server a gratuity.
My family and I loved the Medieval Times Dinner Show and it was worth the wait in traffic and driving home late in the evening. There are shows in several cities across the country and it makes a fun family night out or celebration. I definitely recommend you check them out if there's a Medieval Times near you!
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text:
The Sanborn Identity: Award-winning filmmaker
Sissy Spacek wasn't the only C'ville celeb who made an appearance at last weekend's 18th annual Virginia Film Festival. WINA reporter Bruce Sanborn was also present– but not for his day job.
Sunday afternoon he was at the Regal Theater accepting an award for his full-length screenplay, one of three scripts selected as winners of the annual Governor's Screenwriting Competition, a contest hosted by the Richmond-based Virginia Film Office.
"I've never received an award of this degree before," says Sanborn, "so naturally I'm pleased."
Roughly 90 screenplays were submitted in the statewide competition, but Sanborn's Touch, "a bittersweet romance set in a small town in Virginia," was one of those that stood out.
"What typically sets our winners apart is an original, interesting screenplay," says Virginia Film Office communications manager Mary Nelson. "One of the pitfalls of young writers is that they tend to reproduce genres– but how many more car-chase movies do we need? Our winners, on the other hand, are creative minds at work."
Including Sanborn, who by now knows the ins and outs of the entertainment industry, having acted in Los Angeles and lived in New York as an off-Broadway playwright for nine years before moving to Charlottesville. He's no novice to film writing, either.
"I've written comedies, horror films, dramas," he says. "This particular work is about a mysterious young woman who becomes involved with a shy gardener."
"I think it's a magical story," says local film financier Barry Sisson. "It's one of the best scripts I've ever read."
Sanborn began composing Touch two years ago. And while he says it's a long way from being produced, his fans didn't leave the Festival disappointed. His short film, Uriah had its first public showing Friday, October 28 in UVA's Culbreth Theater.
"It's a great experience to be able to attend a showing of something you've written," says Sanborn of the 10-minute-long work, "especially on the big screen."
Sanborn says he loves the Festival not just because it screened his film but also for the support it provides to independent filmmakers.
"I've started going back to making my own films, including Uriah, because it can be very frustrating working with other people on a single movie," he says. "If you're all working on the same page, it's great. If not, it's not. The downside, of course, is how much extra work is involved. If you see Uriah, you see how many roles I played in creating the film.
"I'll still be making films; in fact, I'll be starting pre-production for my next one this January and February. I'll just be relying on individuals, not filmmaking companies."
Sanborn claims that his plight is common among screenwriters everywhere.
"When it comes to production, we're the low men on the totem pole," he says.
Bruce Sanborn


text:
The Lee Bros. remembered a wedding where one of the Yankee guest helped clean up and in doing so, threw out the potlikker. One favorite use for leftover potlikker is to poach eggs in the liquid the morning after. Alas, no potlikker poached eggs on that day.
Now I am going to share with you two of my favorite uses for potlikker. I am, however, not going to tell you how to cook collards. But be advised, the flavor and strength of the potlikker is directly proportional to the person that made it. Mama's might vary from Grandma's and vice-versa. You want a potlikker that has a nice green color to it and is a bit on the salty side. Great potlikker takes time.
I told the Lee Bros. my favorite use for potlikker was a Potlikkertini. Frankly, there is nothing that can't be improved with a nice shot of vodka. I like to serve them in old-fashioned champagne coupes. They are served warm with a nice tuile of bacon.
A touch of vermouth
3 ounces warm potlikker
1 1/2 ounces Pepper Vodka (it's easy to infuse your own, but Absolut Peppar is fine)
Rinse your glass with vermouth. Mix the vodka and potlikker. Add a bacon garnish.
Now for something more complex.
After the event with the Lee Bros. I was telling Anne that I liked to make a variation on oeufs en gelée with potlikker. Anne said she had some molds she would never use again so, she gave them to me.
It was a lovely night, The Lee Bros., a new cookbook, and new tins!
My reservation about oeufs en gelée is the runny poached egg. The runny cold poached egg that dribbles out on the dish. Here is a very Southern way around that -- Deviled Oeufs en Potlikker Gelée. Yes, take your favorite deviled egg and drop in in aspic.
Deviled Oeufs en Potlikker Gelée
4 small boiled eggs
1 tablespoon mayonnaise
1/2 teaspoon mustard
1/4 teaspoon chopped dill pickles.
2 cups potlikker
1 1/2 teaspoon gelatin
I know it is hard in America to find anything that is small. We love to jumbo-up everything, but try to find the smallest eggs you can. The tins I received from Anne were vintage. If I had used extra-large eggs, there would have been no room for the gelée. In fact, an extra-large egg would have filled the tin and then some. You can use small tins, ramekins, or any mold. Test the size of your tin or mold by placing an egg in its shell into the container. The egg should fit into the tin with about a 1/4 inch around to spare.
Hard boil the eggs. (I always cook and extra egg or two in case one tears.) With deviled eggs, it doesn't matter if you separate them, but with these eggs, it is important to keep the egg halves together as you are going to put the halves back together and a tight fit is best.
Cut the eggs in half, keeping the halves together. Remove the cooked yolk and mash with a fork or, for a finer yolk, run it through a strainer. Add the mayonnaise and mustard and mix into a paste. Add the dill pickles and mix. (This is the way I make deviled eggs, but fell free to make them however your Mama taught you.)
Carefully fill the cavity of each hale of the boiled egg flush with edge. Then put the two halves back together. You do not want any filling squeezing out. I keep a damp towel close by to remove any excess filling .
Place the deviled eggs in the refrigerator until ready to use.
Strain the potlikker several times to remove the fat used to cook the collard and any stray bits of collards or seasonings that may be left behind in the potlikker. A coffee filter over a glass works fine.
When the potlikker is strained, heat 1 1/2 cups in a sauce pan.
In a measuring cup with a spout or a small bowl, add 1/2 cup of the potlikker and sprinkle with the gelatin, stirring to mix.
Add the 1 1/2 cups of hot potlikker to the gelatin mixture and stir. Pour a small amount of the warm potlikker and gelatin into the bottom of each mold, about 1/4 inch. Place the molds and the remaining gelatin in the refrigerator and let the gelatin in the bottom of the mold set, about 10 minutes.
When the gelatin in the molds has set, take the molds, the remaining gelatin and the deviled eggs out to assemble. To each mold, add one deviled egg, keeping the seams on the sides. When the eggs are in place, take the remaining gelatin and give it a quick stir, then carefully pour over the egg, filling the mold.
Return to the refrigerator and allow to set for at least one hour.
Many times, the gelée is decorated in the initial pouring, by adding cut peppers or edible flowers, but the darkness of the potlikker makes that a bit harder.
When you cut in, no runny yolk.
You can see from these pictures that my eggs were a little big for the tins and were not fully covered. It is not really a problem.
So now, you have some ideas of what to do with that leftover potlikker.


text:
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Football Coach Glenn Caruso '96: A Brilliant Mind for Offense
Division III head football coach Glenn Caruso '96 is scoring with his version of the "play action run." by Greg Ryan '08
Ask Glenn Caruso '96 how he learned the nuances of complementary play calling, and the new head football coach of the University of St. Thomas credits hard work, long afternoons practicing football on South Hill's playing fields, and "Bill Walsh College Football '95," a Sega Genesis video game. Glenn and his Bombers teammates would play the game every night after practice — "after homework, too," the onetime sport studies major is quick to add.
If a career average of 32 points per game as an offensive coordinator and head coach, and the cover of American Football Monthly's August 2007 issue are any indication, all those hours spent playing video games paid off.
Glenn is quickly establishing a reputation as one of college football's most brilliant offensive minds. After launching his coaching career as an assistant at North Dakota State University and the University of Wisconsin Eau-Claire, he became the University of South Dakota's offensive coordinator in 2004. In just two years, the Coyotes' scoring average jumped by 29 points per game. In 2006, Glenn earned his first shot at head coaching with Division III Macalester College in St. Paul, Minnesota. Although he inherited a senior class that had won only two games in its first three years ("I swear they weren't even that good"), Glenn led the team to six wins in two seasons and boosted its scoring average from 11 to 28 points per game.
Glenn credits much of his success to his version of the "play action run," in which his offensive players begin select plays as if the quarterback is going to pass, then quickly switch gears and run the ball, leaving defensive players confused and off balance. For decades teams have been using such pass fakes sporadically, but Glenn has made them a focal point of his offense, with play action runs making up 25 percent of his rushing attack.
The system's stunning effectiveness leaves onlookers wondering from what coaching legend Glenn learned to call plays. "Reporters would always ask, 'Are you from the Bill Walsh, Steve Spurrier, or Urban Meyer tree?' " Glenn says, "I'd say, Nope — I'm from the Jim Butterfield tree," referring to the legendary Bombers coach under whom Glenn played as a freshman and sophomore.
This fall Glenn will take his offensive fireworks show just down the road from Macalaster, to Division III St. Thomas (where new IC president Thomas Rochon served as executive vice president and chief academic officer for five years before coming to Ithaca). The Bombers' former starting center says he'll continue to draw from the lessons he learned during his playing days at IC. "There's no doubt the concepts I was taught in Ithaca are what allow me to see the bigger picture of the game today," he says. Video games helped, too.
1 Comment
Glenn Caruso is one of the finest men I have ever met. With his help, I have incorporated the Pass Action Run into my offensive schemes and learned to take advantage of defensive stress values. Thank God there is a man like Glenn to lead the way!


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The second thing I did was to add more shadows and add more colour in the shadow parts. This will give it more depth then just a simple gray layer.
After finishing most of the shadow parts I started in one corner to layer colours and blend them together. Added more details to it.
And that's where I am right now. Hopefully I can do a bit more today, although it is very warm today. We're playing outside most of the time today. It's okay to sit in the shadow under the trees and Bertus can play with water there.
Veronicastrum virginicum 'Diana' is a smaller variety of my Veronicastrums. While the other, taller ones have barely any flowers left, this white beauty is just starting to bloom. It is standing in a spot where is more shadow. I guess that's the reason why.
Another thing I noticed today is my Rosa Glauca. She thinks that it's almost autumn so it seems. The rose hips are starting to turn red and dark, the leaves are turning yellow.
It's all going so fast in this dry and hot weather... Thankfully an other rose thinks it's springtime. 'Moonlight' is getting a lot of red young, fresh shoots and leaves. Beautiful to see it when the sun is shining through.


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Anne, Queen of Great Britain
Date: 1665 - 1714
Remarks: Anne, the last Stuart monarch, took to the throne of England, Ireland and Scotland in 1702. In 1707, the Act of Union was passed, uniting England, Scotland and Wales into Great Britain, making Anne the first Queen of Great Britain. Her reign was dominated by the War of Spanish Succession, (known in America as the French and Indian Wars). It was during her reign that artists, writers and thinkers such as Sir Christopher Wren, Sir Isaac Newton, Swift and Pope were active. - Source: http://www.bartleby.com/65/an/AnneQueen.html


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versión On-line ISSN 1851-8044
Ameghiniana v.45 n.1 Buenos Aires ene./mar. 2008
Paleoecological and paleoenvironmental implications of a high-density Chondrites association in slope deposits of the Neogene Santo Domingo Formation, Valdivia, south-central Chile
Alfonso Encinas1, Luis A. Buatois2 and Kenneth L. Finger3
1Departamento de Ciencias de la Tierra, Universidad de Concepción, Casilla 160-C, Chile. firstname.lastname@example.com
2Department of Geological Sciences, University of Saskatchewan, 114 Scence Place, Saskatoon, SK S7N 5E2, Canada. firstname.lastname@example.com
3University of California Museum of Paleontology, 1101 Valley Life Sciences Building, Berkeley, CA 94720-4780, USA. email@example.com
Abstract. Neogene marine strata of the Santo Domingo Formation crop out in the vicinity of Valdivia, south-central Chile (40°S, 73°W). The succession is characterized by dark-gray sandy siltstone with abundant Chondrites isp. The occurrence of this ichnotaxon and lower-bathyal benthic foraminifers is consistent with a slope depositional environment. The abundance of Chondrites and the low ichnodiversity reveal poorly oxygenated bottom waters. The Santo Domingo Formation most likely accumulated in fault-controlled, intraslope silled minibasins, which werw formed during a major event of Neogene subsidence of the Chilean margin.
Resumen. Implicancias Paleoecológicas Y Paleoambientales De Una Asociación De Alta Densidad De Chondrites En Depósitos De Talud De La Formación Santo Domingo, Neógeno De Valdivia, Centro-Sur De Chile. Estratos marinos Neógenos pertenecientes a la Formación Santo Domingo afloran en los alrededores de Valdivia, Chile centro-sur (40°S, 73°W). Dicha sucesión se caracteriza por la presencia de limolitas arenosas de color gris oscuro con abundantes Chondrites isp. La presencia de este icnotaxón y de foraminíferos bentónicos característicos de profundidades batiales inferiores indicarían que la sedimentación de esta unidad se produjo en un ambiente de talud. La abundancia de Chondrites y la baja icnodiversidad sugiere que las aguas del fondo marino estaban pobremente oxigenadas. Se propone que la Formación Santo Domingo se depositó en pequeñas cuencas de talud controladas por fallas que se formaron como consecuencia de un importante evento de subsidencia del margen chileno.
Key words. Ichnology; Trace fossils; Chondrites; Slope; Neogene; Chile.
Palabras clave. Icnología; Trazas fósiles; Chondrites; Talud; Neógeno; Chile.
Neogene marine strata crop out around the city of Valdivia, in the coastal area of south-central Chile (40°S, 73°W) (figure 1). These deposits were first studied by Brüggen (1950) who correlated this succession with the Navidad Formation, the reference unit for the marine Neogene of Chile (Cecioni, 1980). Subsequently, Martínez-Pardo and Pino (1979) defined these strata as the Santo Domingo Formation in their study of the homonym roadcut section located approximately 19 km southeast of Valdivia.
Figure 1. Location map, showing localities cited in the text and the outline of the outcrops of the Santo Domingo Formation. Map modified from Sernageomin 1998 / mapa de ubicación en que semuestran las localidades citadas en el texto y los afloramientos de la Formación Santo Domingo. Mapa modificado de Sernageomin 1998.
The Valdivia area is one of several Chilean coastal localities where Neogene marine strata crop out (e.g., Cecioni, 1980; Le Roux et al., 2005; Encinas et al., 2006). These strata have also been recognized in boreholes drilled on the continental shelf of southcentral Chile (Mordojovich, 1981). In the area located approximately between the cities of Temuco and Puerto Montt (38°30'-41°30'S), Neogene marine strata also crop out in the Central Valley and even in the westernmost part of the Main Andean Cordillera (Osorio and Elgueta, 1990; Elgueta et al., 2000). Strata belonging to the Santo Domingo Formation have been interpreted as having been deposited in deep-marine embayments (Chirino-Gálvez, 1985; Le Roux and Elgueta, 2000; Elgueta et al., 2000).
However, Cecioni (1970) and Martínez-Pardo and Pino (1979) mentioned the presence of bathyal species of benthic foraminifera, and Covacevich et al. (1992) noted the occurrence of Chondrites isp., an ichnogenus that, although not exclusive, is commonly abundant in outer shelf and continental slope deposits (Frey and Pemberton, 1984). In addition, studies recently carried out on correlative Neogene units exposed in the Navidad (34°S), Arauco (37°S) and Chiloé (42°S) areas, and previously considered as shallow-marine successions (e.g., Cecioni, 1978; Cecioni, 1980), indicate that they were deposited at lower bathyal (2000-4000 m) depths (Finger et al., 2007; Encinas et al., in press). This encourages us to carry out sedimentologic, ichnologic, and micropaleontologic analyses to try to unravel the depositional environment and paleobathymetry of the Santo Domingo Formation.
Since the pioneering studies of Seilacher (1967), ichnologists have utilized trace fossils as paleobathymetric indicators. Yet, such interpretations must be made with caution, as water depth is only a secondorder controlling factor in the distribution of trace fossils and ichnofacies (Frey et al., 1990). It is well known that other parameters, such as hydrodynamic energy, substrate, oxygen content, and food supply, effectively modify Seilacher's classical scheme (Frey et al., 1990; Pemberton et al., 1992). Fortunately, these factors generally vary in accordance with water depth, which renders ichnology a very useful tool in the determination of paleobathymetry and onshoreoffshore trends, particularly when combined with sedimentologic and paleontologic analyses (e.g. Mac- Eachern et al., 1999; Mángano et al., 2005). In the present study, we use ichnologic and micropaleontologic evidence from the type locality of the Santo Domingo Formation in order to evaluate the paleoenvironmental implications of abundant Chondrites in these deposits.
Geologic setting
The area located around Valdivia has a basement of Paleozoic metamorphic rocks and minor Cretaceous granitoids overlain by an Oligocene?-early Miocene? continental-paralic coal-bearing succession of the Pupunahue-Catamutún Formation, Miocene marine deposits of the Santo Domingo Formation, and Pleistocene-Holocene glacial, marine, and fluvial deposits (Sernageomin, 1998).
The Santo Domingo Formation unconformably overlies the Paleozoic metamorphic rocks of the Bahía Mansa complex (Sernageomin, 1998). It also overlies the Pupunahue-Catamutún formation, although it is not clear whether the contact with this unit is gradational (Elgueta et al., 2000) or if there is a discontinuity, as suggested by the abrupt transition from a coal-bearing unfossiliferous succession to a silty, fossil-rich unit that can be observed in boreholes drilled at the Catamutún mining area southeast of Valdivia (Alfaro et al., 1990). Although the maximum thickness of this unit at Cuesta Santo Domingo (figure 1) is 110 m, this must be considered as a minimum estimate because there is no place where a complete section can be measured. The basal part of the Santo Domingo Formation can only be observed in a limited number of places, such as the coastal cliffs located immediately north of Corral (figure 1). It consists in a succession of schist breccia with minor sandstone. The basal breccia is overlain by a succession of dark-gray sandy siltstone, which constitute the most characteristic facies of this unit, and minor sandstone and breccia. At Cuesta Santo Domingo, neither the basal contact nor the basal interval are visible and only a succession of sandy siltstone is exposed. The Santo Domingo Formation contains a fossil biota that includes bivalves, gastropods, brachiopods, bryozoans, crustaceans, echinoids, fishes, foraminifers, ostracodes, radiolarians and leaves (Chirino-Gálvez, 1985; Pino and Beltrán, 1979; Martínez- Pardo and Pino, 1979; Covacevich et al., 1992). Martínez-Pardo and Pino (1979) assigned a late middle Miocene (N13-N15 zones) to this unit based on their study of foraminifers from Cuesta Santo Domingo (figure 1). However, this age determination, considered to be a problematic approach because benthic foraminifers biostratigraphic ranges are facies controlled and therefore time-transgressive as opposed to those of fossil plankton (Ingle, 1980).
Martínez-Pardo and Pino (1979) recorded eight species of planktic foraminifers, but all were identified with uncertainty as indicated by the "cf." (confer with) modifier. It is probably safe to assume that the forms they recorded as Globigerinoides cf. trilobus and Globorotalia cf. continuosa belong to those species, which have a concurrent range from zone N9 to zone N16 (Middle to Late Miocene). In the Catamutún area, approximately 40 km south of Valdivia, marine beds stratigraphically equivalent to the Santo Do- mingo Formation were assigned a middle Miocene (Langhian-Serravallian, zones N10-N12) age by Marchant and Pineda (1988) and Marchant (1990). Although their determinations also were based partially on benthic foraminifers, they recorded the planktic foraminifer Globigerina pachyderma, which has its first appearance datum in N16 and thus indicates a maximum age of Tortonian (Late Miocene). This correlates with the late Miocene-early Pliocene ages determined for the Navidad, Ranquil, and Lacui formations exposed in the areas of Navidad, Arauco, and Chiloé, respectively (Finger et al., 2007; Encinas et al., in press). We therefore ascribe a probable late Miocene age to the Santo Domingo Formation, although we do not discard a broader age range. Additional data is needed to accurately constrain the age of this unit.
The Cuesta Santo Domingo succession: outcrop description, associated trace fossils and foraminiferal assemblages
Our study was focused on the sedimentary succession that crops out at Cuesta Santo Domingo (39°56'S-73°07'W) (figure 1), considered as the type locality of the homonym Formation (Martínez-Pardo and Pino, 1979). Studies were focused on this locality due to the relatively good preservation of invertebrate trace and body fossils. Other roadcut and coastal outcrops west and south of Valdivia where also examined. They show similar sedimentary facies, trace fossils and microfossil content but with a poorer preservation.
The Cuesta Santo Domingo is located along the road between Valdivia and Paillaco, approximately 19 km southwest of Valdivia (figure 1). It starts approximately 300 m southwest of the road exit to Corral and continues along 2 km. Exposures along the edge of the road are intermittent due to high vegetation cover. They are 2 to 6 m in height, except for one of the of the basal part of the section that is 25 m in height on the hillside of a farm near the deviation to Corral (figure 2). The sedimentary succession of Cuesta Santo Domingo consists almost exclusively of sandy siltstone; a few medium-grained sandstone beds are also present. The siltstone is dark gray when fresh and light gray to orangebrown when weathered. It is slightly fissile, massive, and usually breaks in large blocks. No clear bedding planes were observed. Bivalves, gastropods, crustaceans, and echinoderms are common. Although the metamorphic basement is observed in some outcrops near the base of the succession, the basal contact of the Santo Domingo Formation is not exposed.
Figure 2. Typical aspect of sandy siltstone facies of the Santo Domingo Formation at Cuesta Santo Domingo. Cliff is approximately 25 m high / aspecto típico de las facies de limolitas arenosas de la Formación Santo Domingo en la Cuesta Santo Domingo. El escarpe mide aproximadamente 25 m de altura.
The benthic foraminiferal assemblage that we recorded from this unit is much more diverse than that recorder in Martínez-Pardo and Pino's (1979) list, and it includes both shallow- and deep-water indicators. The bathyal component of the assemblage includes Bathysiphon sp., Bulimina spicata, Favulina hexagona, Glandulina laevigata, Globobulimina galliheri, Hansenisca soldanii, Hanzawaia concentrica, Hoeglundina elegans, Oridorsalis umbonatus, Pullenia bulloides, Martinottiella communis, Melonis pompilioides, Nodosaria longiscata, Pseudonodosaria torrida, Rectuvigerina transversa, and Sphaeroidina bulloides. The assemblage also includes many shallow-water indicators; thus, it is mixed-depth association that indicates downslope displacement. Melonis pompilioides is generally considered to be a cosmopolitan indicator of lower-bathyal (2000 to 4000 m) depths (e.g., Ingle, 1980; Morkhoven et al., 1986; Finger et al., 2007); Bathysiphon sp. and Nodosaria longiscata are also indicative of this depth zone off Chile (see Bandy and Rodolfo, 1964; Ingle et al., 1980).
Chondrites isp. is extremely abundant in these deposits. This ichnotaxon was observed after breaking siltstone blocks along fissile planes. No clear bedding planes were observed jutting out as the result of differential erosion, which likely would have facilitated the preservation of traces. The trace fossils are clearly distinguishable only in weathered rocks because they conserve the original gray color that contrasts with the more altered brown matrix. Partially preserved spreiten structures similar to Zoophycos are also present, but their accurate identification is not possible due to their fragmentary preservation. Chondrites isp. consists of straight to slightly curved, regularly branching systems. The tunnels are approximately 0.8 mm wide (figure 3). The angle of branching is less than 45°. Only second-order branches were observed. Specimens are abundant and can be clearly distinguished in oxidized siltstone because the internal filling is pristine and preserves its original gray color. No attempts have been made to classify Chondrites at ichnospecific level because the status of most of its ichnospecies is still uncertain. Some curved segments resemble Nereites missouriensis, but lack the typical backfill of this ichnotaxon.
Figure 3. Chondrites isp. from the Santo Domingo Formation. Scale bar = 1 cm. A) Typical Chondrites branching is observed below the scale. B) Radial pattern and typical branching is observed below the scale / Chondrites isp. de la Formación Santo Domingo. Barra de escala = 1 cm. A) La ramificación característica de Chondrites se puede observar bajo la escala. B) El diseño radial y la ramificación característica se puede observar bajo la escala.
Chondrites is generally considered to be a feeding system of unidentified infaunal deposit-feeders (e.g., Osgood, 1970). However, according to Seilacher (1990) and Fu (1991), the tracemaker of Chondrites may be able to live in the aerobic/anoxic interface as a chemosymbiotic organism that pumps methane and hydrogen sulphide from the sediments, whereas Kotake (1992) suggested the possibility that this trace is merely a "cess-pit" for fecal pellets produced by the excretory behavior of surface deposit feeders. Monospecific assemblages of Chondrites suggest poorly oxygenated bottom waters (e.g., Fu, 1991; Bromley, 1996). For example, Chondrites is the dominant ichnospecies on the northern slope of the Iceland- Faero Ridge, where sluggish bottom currents, organic-rich sediments, and oxygen deficiency prevails (Fu and Werner, 1994). Baas et al. (1998) found massive occurrences of Chondrites during halted or reduced thermohaline circulation leading to lowered oxygenation levels of the bottom waters in the eastern North Atlantic. Löwemark et al. (2004) observed the massive occurrence of this ichnogenus in Holocene sediments of the southwestern Iberian continental slope during the onset of low current velocities and enhanced deposition of particulate organic matter leading to low pore-water oxygen levels. Uchman et al. (2003) found Chondrites in laminated micrite that fills deep submarine cavities in peri-reefal biocalcarenite and calcirudite of the Tithonian-Berriasian Stramberg Limestone (Czech Republic) in a very stressful, low-oxygen environment. In shallow-water settings, extremely dense concentrations of Chondrites were linked to burial of high quantities of organic matter during storm events (Vossler and Pemberton, 1988).
The association of Chondrites and forms resembling Zoophycos compare favorably with the Zoophycos ichnofacies, which is typical, although not exclusive, of outer shelf to slope settings (Frey and Pemberton, 1984). Although this ichnofacies is placed between the sublittoral and the abyssal zones in Seilacher's (1967) popular bathymetric scheme, it also occurs in shallower-water, epeiric deposits, particularly during the Paleozoic (e.g., Miller, 1991). This is because one of the main environmental controls of this ichnofacies is lowered oxygen levels associated with abundant organic material in quiet-water settings (Frey and Seilacher, 1980). However, uncertainties regarding an accurate identification of Zoophycos complicate ichnofacies assessments. Regardless of ichnofacies identification, benthic foraminifers in the Santo Domingo succession also support a deep-marine depositional environment.
A trace fossil association similar to that described here for the Santo Domingo Formation is recognized in the correlative Navidad Formation (Encinas et al., in press). However, there are some differences between the trace fossil assemblages that characterize both units. Two different ichnofacies have been recognized in the Navidad Formation: the Zoophycos ichnofacies, found in siltstone and very fine-grained sandstone, and the Skolithos ichnofacies that occurs mostly in massive, medium- to coarse-grained sandstone. The Zoophycos ichnofacies characterizes calm, low sedimentation intervals whereas the Skolithos ichnofacies reflects short-term, high-energy conditions associated with the sudden deposition of thick packages of sand (Encinas et al., in press). In contrast, the Skolithos ichnofacies has not been recognized in the Santo Domingo Formation. This is probably due to the scarcity of sandy intervals that this unit shows in contrast with the Navidad Formation that presents abundant coarsed-grained intervals. Another difference between these units is that the Zoophycos ichnofacies in the Navidad Formation is a more diverse association that includes Chondrites isp., Zoophycos isp., Lophoctenium isp., Diplocraterion parallelum and Planolites isp. (Encinas et al., in press). In addition, Chondrites is not as abundant as in the Santo Domingo Formation. However, this could be due to differences in outcrop quality. The Navidad Formation occurs as continuous and well-preserved exposures along several kilometers of coastal bluffs, while the Santo Domingo Formation crops out in a more limited number of roadcuts and coastal outcrops because the wetter climate of the Valdivia area supports a thicker vegetational cover. Nevertheless, the consistent and widespread occurrence of Chondrites-bearing gray siltstone facies in most outcrops of the Santo Domingo Formation, some of them several tens of meters thick, suggests that the ichnologic and lithologic differences between this unit and the Navidad Formation reflect more than just differences in outcrop quantity and quality.
The abundance of Chondrites and the presence of lower-bathyal benthic foraminifers in the type locality of the Santo Domingo Formation are consistent with a deep-marine depositional environment for this unit. Sedimentologic and paleontologic studies carried out in Neogene marine deposits that crop out in several areas along the Chilean coastline also indicate bathyal depositional depths for at least part of these successions (Le Roux et al., 2005; Finger et al., 2007; Encinas et al., in press). Deep-marine sedimentation in these areas has been attributed to forearc subsidence caused by a major event of tectonic erosion that affected the Chilean margin during the Neogene (Encinas et al., in press). Hence, the Santo Domingo Formation provides evidence of this tectonically- induced transgression for the Valdivia area. The ichnofauna of the Santo Domingo Formation suggests deposition in poorly oxygenated bottom waters. Further evidence of low-oxygen conditions are the abundance of black siltstone intervals, the occurrence of pyrite in this succession (Chirino-Gálvez, 1985) and geochemical analysis that show V/(V/Ni) rates of 0.75 (Bravo, 2006). A possible explanation for anoxic conditions during sedimentation of the Santo Domingo Formation is that this unit was deposited in fault-controlled, silled, intra-slope minibasins similar to those of the California Borderland and the modern Guaymas Basin in the Gulf of California (Ingle, 1981).
If the depth of the sill is within the oxygen-minimum layer, all of the water below sill depth will be oxygen deficient regardless of the maximum depth of the basin floor (Ingle, 1981). Silled intra-slope minibasins commonly display limited deep-water circulation, leading to depauperate trace fossil assemblages due to oxygen-depleted conditions (Mángano and Buatois, 1997). In addition, open-ocean surface currents bearing planktic foraminifers may be restricted from some silled basins, which could explain relatively small ratios of planktic vs. benthic foraminifers (Martínez- Pardo and Pino, 1979). In contrast, partially ponded intra-slope minibasins contain more diverse ichnofaunas, although the Nereites ichnofacies is absent (e.g. Schultz and Hubbard, 2005).
The Neogene Santo Domingo Formation that crops out near Valdivia contains abundant Chondrites isp. The presence of this ichnogenus and a mixed-depth assemblage of benthic foraminifers that includes lower- bathyal indicators indicate a deep-water depositional environment. In addition, the low diversity of the trace association and the abundance of Chondrites characterize poorly-oxygenated bottom waters. It is suggested that the Santo Domingo Formation was deposited in fault-controlled, silled, deep-marine basins during a significant event of forearc subsidence resulting from tectonic erosion of the margin.
AE was supported by Proyecto Fondecyt No. 3060051 of Conicyt and the IRD (Institut de Recherche pour le Développment). LB was supported by a NSERC Discovery Grant 311726-05. We gratefully thank their financial help to these institutions. We also would like to thank G. Hérail, M. Pino and S. Villagrán for their help. We finally thank E.B. Olivero and M. Verde for reviewing the paper.
1. Alfaro, G., Gantz, E. and Magna, O. 1990. El yacimiento de carbón Catamutún (La Unión). 2º Simposio sobre el Terciario de Chile (Concepción), pp. 11-28. [ Links ]
2. Baas, J.H., Schönfeld, J. and Zahn, R. 1998. Mid-depth oxygen drawdown during Heinrich events: Evidence from benthic foraminiferal community structure, trace fossil tiering, and benthic d13C at the Portuguese margin. Marine Geology 152: 25- 55. [ Links ]
3. Bandy, O.L. and Rodolfo, K.S. 1964. Distribution of foraminifera and sediments, Peru-Chile Trench area. Deep-Sea Research 1: 817-837. [ Links ]
4. Bravo, M.J. 2006. [Evolución geoquímica de la cuenca de Mulpún- Pupunahue, X Región de los lagos, Chile. Graduate Thesis, Departamento de Ciencias de la Tierra de la Universidad de Concepción, Concepción, 71 pp. Unpublished.]. [ Links ]
5. Bromley, R.G. 1996. Trace Fossils: Biology, Taphonomy and Applications. Chapman and Hall, London, 361 pp. [ Links ]
6. Brüggen, J. 1950. Fundamentos de la Geología de Chile. Instituto Geográfico Militar. Santiago, Chile, 374 pp. [ Links ]
7. Chirino-Gálvez, L. 1985. Paleoecología del bentos del Mioceno marino de Valdivia. 4° Congreso Geológico Chileno (Antofagasta), Actas 1: 133-135. [ Links ]
8. Cecioni, G. 1970. Esquema de Paleogeografía Chilena. Editorial Universitaria, Santiago de Chile, 143 pp. [ Links ]
9. Cecioni, G. 1978. Petroleum possibilities of the Darwin's Navidad Formation near Santiago, Chile. Publicación Ocasional del Museo Nacional de Historia Natural de Chile 25: 3-18. [ Links ]
10. Cecioni, G. 1980. Darwin's Navidad embayment, Santiago region, Chile, as a model of the southeastern Pacific shelf. Journal of Petroleum Geology 2-3: 309-321. [ Links ]
11. Covacevich, V., Frassinetti, D. and Alfaro, G. 1992. Paleontología y condiciones de depositación del Mioceno marino en las nacientes del río Futa, Valdivia, Chile. Boletín del Museo Nacional de Historia Natural de Chile 43: 143-154. [ Links ]
12. Elgueta, S., McDonough, M., Le Roux, J., Urqueta, E. and Duhart, P. 2000. Estratigrafía y sedimentología de las cuencas terciarias de la Región de Los Lagos (39-41°30'S). Boletín de la Subdirección Nacional de Geología 57: 1-50. [ Links ]
13. Encinas, A., Le Roux, J.P., Buatois, L.A., Nielsen, S.N., Finger, K.L., Fourtanier, E. and Lavenu, A. 2006. Nuevo esquema estratigráfico para los depósitos marinos mio-pliocenos del área de Navidad (33°00'-34°30'S), Chile central. Revista Geológica de Chile 33: 221-246. [ Links ]
14. Encinas, A., Finger, K., Nielsen, S., Lavenu, A., Buatois, L., Peterson, D. and Le Roux, J.P. In press. Rapid and major coastal subsidence during the late Miocene in south-central Chile. Journal of South American Earth Sciences. Doi: 10.1016/j.jsames.2007.07.001. [ Links ]
15. Finger, K.L., Nielsen, S.N., DeVries, T.J., Encinas, A. and Peterson, D.E. 2007. Paleontologic evidence for sedimentary displacement in Neogene forearc basins of central Chile. Palaios 22: 3- 16. [ Links ]
16. Frey, R.W. and Seilacher, A. 1980. Uniformity in marine invertebrate ichnology. Lethaia 13: 183-207. [ Links ]
17. Frey, R.W. and Pemberton, S.G. 1984. Trace fossils facies models. In: R.G. Walker (ed.), Facies Models. Geoscience Canada Reprints Series, pp. 189-207. [ Links ]
18. Frey, R.W., Pemberton, S.G. and Saunders, T.D.A. 1990. Ichnofacies and bathymetry: a passive relationship. Journal of Paleontology 64: 155-158. [ Links ]
19. Fu, S. 1991. Funktion, Verhalten und Einteilung fucoider und lophocteniider Lebenspuren. Courier Forschungsinstitut Senckenberg, Senckenbergischen Naturforschende Gesellschaft, Frankfurt a.M., pp. 1-79. [ Links ]
20. Fu, S. and Werner, F. 1994. Distribution and composition of biogenic structures on the Iceland-Faeroe Ridge: relation to different environments. Palaios 9: 92-101. [ Links ]
21. Ingle, J.C.Jr. 1980. Cenozoic paleobathymetry and depositional history of selected sequences within the southern California continental borderland. In: V. William, V. Sliter, J.C. Ingle, J.P. Kennet, R. Kolpack, E. Vincent (eds.), Studies in Marine Micropaleontology and Paleoecology. A Memorial Volume To Orville, L. Bandy. Cushman Foundation for Foraminiferal Research, Special Publication 19: 163-195. [ Links ]
22. Ingle, J.C., Jr., Keller, G. and Kolpack, R. 1980. Benthic foraminiferal biofacies, sediments and water masses of the southern Peru-Chile Trench area, southeastern Pacific Ocean. Micropaleontology 26: 113-150. [ Links ]
23. Ingle, J.C.Jr. 1981. Origin of Neogene diatomites around the North Pacific rim. In: R.E. Garrison, R.G. Douglas (eds.), The Monterrey Formation and Related Siliceous Rocks of California. Society of Economic Paleontologists and Mineralogists, pp. 159-179. [ Links ]
24. Kotake, N. 1992. Deep-sea echiurans: possible producers of Zoophycos. Lethaia 25: 311-316. [ Links ]
25. Le Roux, J.P. and Elgueta, S. 2000. Sedimentologic development of a Late Oligocene-Miocene forearc embayment, Valdivia Complex, southern Chile. Sedimentary Geology 130: 27-44. [ Links ]
26. Le Roux, J.P., Gómez, C., Venegas, C., Fenner, J., Middleton, H, Marchant, M., Buchbinder. B., Frassinetti, D., Marquardt, C., Gregory-Wodzicki, K.M. and Lavenu, A. 2005. Neogene- Quaternary coastal and offshore sedimentation in north-central Chile: record of sea level changes and implications for Andean tectonism. Journal of South American Earth Sciences 19: 83-98. [ Links ]
27. Löwemark, L., Schönfeld, J., Werner, F. and Schäfer, P. 2004. Trace fossils as a paleoceanographic tool: evidence from late Quaternary sediments of the southwestern Iberian margin. Marine Geology 204: 27-41. [ Links ]
28. MacEachern, J.A., Zaitlin, B.A. and Pemberton, S.G. 1999. A sharp-based sandstone of the Viking Formation, Joffre Field, Alberta, Canada: criteria for recognition of transgressively incised shoreface complexes. Journal of Sedimentary Research Section B 69: 876-892. [ Links ]
29. Mángano, M.G. and Buatois, L.A. 1997. Slope apron deposition in an Ordovician arc-related setting, Chaschuil area, Famatina Basin, Northwest Argentina. Sedimentary Geology 109: 155-180. [ Links ]
30. Mángano, M.G., Buatois, L.A. and Muniz Guinea, F. 2005. Ichnology of the Alfarcito Member (Santa Rosita Formation) of northwest Argentina: Animal-substrate interactions in a lower Paleozoic wave-dominated shallow sea. Ameghiniana 42: 641-668. [ Links ]
31. Marchant, M. 1990. Foraminíferos Miocénicos de los Estratos de Pupunahue (Provincia de Valdivia: X Región): Determinación de la edad probable y paleoambiente. 2º Simposio sobre el Terciario de Chile (Concepción), pp. 177-188. [ Links ]
32. Marchant, M. and Pineda, V. 1988. Determinación de la edad del miembro superior marino de los estratos de Pupunahue, mediante foraminíferos. 5° Congreso Geológico Chileno (Santiago), Actas: C311-C325. [ Links ]
33. Martínez-Pardo, R. and Pino, M. 1979. Edad, paleoecología y sedimentología del Mioceno marino de la Cuesta Santo Domingo, Provincia de Valdivia, X Región. 2° Congreso Geológico Chileno (Arica), Actas: H103-H124. [ Links ]
34. Miller, M.F. 1991. Morphology and environmental distribution of Paleozoic Spirophyton and Zoophycos: Implications for the Zoophycos Ichnofacies. Palaios 6: 410-425. [ Links ]
35. Mordojovich, C. 1981. Sedimentary basins of Chilean Pacific offshore. In: Energy resources of the Pacific region. American Association of Petroleum Geologists, Studies in Geology 12: 63-68. [ Links ]
36. Morkhoven, F.P.C.M. van, Berggren, W.A. and Edwards, A.S. 1986. Cenozoic cosmopolitan deep-water benthic foraminifera. Bulletin des Centres de Recherches Exploration-Production Elf-Aquitaine, Memoire 11: 421 pp. [ Links ]
37. Osgood, R.G.Jr. 1970. Trace fossils of the Cincinnati area. Palaeontographica Americana 6: 277-444. [ Links ]
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39. Pemberton, S.G., MacEachern, J.A. and Frey, R.W. 1992. Trace fossils facies models: environmental and allostratigraphic significance. In: R.G. Walker, N.P. James (eds.), Facies Models, response to sea level change, pp. 47-72. [ Links ]
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41. Schultz, M.R. and Hubbard, S.M. 2005. Sedimentology, stratigraphic architecture, and ichnology of gravity-flow deposits partially ponded in a growth-fault controlled slope minibasin, Tres Pasos Formation (Cretaceous), southern Chile. Journal of Sedimentary Research 75: 440-453. [ Links ]
42. Seilacher, A. 1967. Bathymetry of trace fossils. Marine Geology 5, 413-428. [ Links ]
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Recibido: 24 de mayo de 2007.
Aceptado: 11 de diciembre de 2007.


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Giving NASA a strong dose of stability and direction would help sustain United States leadership in spaceflight and exploration for decades to come, a new report advises.
NASA has been pulled in too many directions for too long, according to the report, which was released Tuesday by the nonprofit Space Foundation. The agency needs to set a unified, long-term vision and be able to work toward it no matter which way the winds of power are blowing in Washington, D.C.
"We think that if you've got your purpose clear, then it becomes easier for you to sit down and detail a 10-year plan and a 30-year plan that you stick to and revisit and revise as you make discoveries," said Space Foundation Chief Executive Officer Elliot Pulham.
A pioneering space agency
In many people's minds, today's NASA is a far cry from the world-beating agency that put a man on the moon in 1969, just 12 years after the Space Age dawned. [ Lunar Legacy: 45 Apollo Moon Mission Photos ]
Neil Armstrong 's famous first steps on the lunar surface were made possible by a laserlike, agencywide focus that just doesn't exist at NASA today, according to the report.
"As the space program has evolved, we have witnessed frequent redirection and constantly shifting priorities at NASA, mixed signals from Congress and the administration, organizational conflicts and the lack of a singular purpose, resulting in a space agency without a clear, stable direction," the report states.
The report argues that NASA needs a unified purpose again. And it recommends what that purpose should be: pioneering. (The report's title is "Pioneering: Sustaining U.S. Leadership in Space.")
"This report does not advocate for space settlement or colonization; rather, it is focused on expanding the human sphere of influence," the authors write. "For example, much of the ocean floor is part of the human sphere of influence through the use of robotics, even if it is seldom visited by humans. One way or another, humans should seek to sustain a presence elsewhere in the solar system."
Pioneering has four phases, as laid out in the report: access (the ability to get to and from a destination); exploration; utilization; and transition (handing activities off when appropriate to other government agencies or to the private sector).
The report stops short of prescribing a particular sequence of destinations.
"We did not want to be in the business of specifying, 'Look, we've got to go to the moon first, we've got to go to Mars first, we've got to do this or that,'" Pulham told Space.com. "Our view is that, if you're pioneering, then you're going to first of all take a much broader survey of the whole solar system, and then the destinations and the order of battle will become pretty clear."
Space news from NBCNews.com
Teen's space mission fueled by social media
Science editor Alan Boyle's blog: "Astronaut Abby" is at the controls of a social-media machine that is launching the 15-year-old from Minnesota to Kazakhstan this month for the liftoff of the International Space Station's next crew.
- Buzz Aldrin's vision for journey to Mars
- Giant black hole may be cooking up meals
- Watch a 'ring of fire' solar eclipse online
- Teen's space mission fueled by social media
Making it happen
The report further recommends that NASA draw up a 30-year plan to map out broad objectives, and a sequence of 10-year plans that set specific dates and commitments within the larger pioneering framework. These plans would be submitted to Congress for approval every five years.
NASA's plans should be vetted by a newly created, 12-person NASA Commission, the report continues. The commission would consist of the space agency chief, three presidential appointees and four members each from the House and Senate.
Implementing a long-term vision requires greater stability in NASA leadership and funding, according to the "Pioneering" report. So the NASA administrator should be appointed to a renewable five-year term (rather than serve at the pleasure of the president), and Congress should create a revolving fund the agency can draw from to finance its operations (instead of simply giving NASA a rigid top-line budget every year).
"We think that NASA's budget needs to be able to fluctuate with the work that they need to do," Pulham said. "The budget needs to track with the program. So we recommended things like multi-year procurement authorizations — something that the Pentagon and other agencies do very successfully."
Pulham does not necessarily expect the report's recommendations to be embraced fully and implemented immediately. But he does hope "Pioneering" gets people talking.
"I'm optimistic that this is going to make a positive contribution to the national dialogue," Pulham said. "If it can serve as nothing more than a point to kick off a national dialogue that does have some result, then we're going to feel really great about what we've done."
Follow Space.com senior writer Mike Wall on Twitter @michaeldwall or Space.com @Spacedotcom. We're also on Facebook and Google+.
- NASA's 2013 Budget: What Will It Buy?
- NASA's 10 Greatest Science Missions
- Visions of the Future of Human Spaceflight
© 2013 Space.com. All rights reserved. More from Space.com.


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When you've been smoking as long as Mortal Kombat's resident grey ninja has been smoking, there's really only one way to kick the habit.
As a filthy smoker and professional martial artist, this would be one of those videos that haunts me to my dying day. Fortunately I am not a professional martial artist, so I'm fine with this.
For more sick and twisted video game comedy, follow the link to Dorkly.com.


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Representative Dean Fisher (R-Garwin) has announced he will seek re-election to the Iowa House. Fisher, who is in his first term, represents all of Tama County and portions of Marshall and Black Hawk Counties.
During his tenure in the House, Fisher has worked to reduce Iowans' taxes, rein in out of control government spending while funding Iowans priorities, and strengthening Iowa's economic climate.
He has also been an outspoken advocate of the Iowa Juvenile Home. Fisher is committed to continuing his work in these areas.
Article Photos
State Representative Dean Fisher
"I am working to protect Iowans' pocketbooks against those in Des Moines who have an insatiable appetite for spending. I believe it's Iowans money first, not the government's and I will do what I can to send more of it back where it belongs, in the hands of the hardworking taxpayers," said Fisher.
"I am also very disappointed in the closing of the Iowa Juvenile Home and it is my hope that, for the sake of these troubled teens, the Legislature has the opportunity to weigh in on this important issue," Fisher said.
Upon graduation from South Tama High School, he received a Bachelor's Degree in Electronics Engineering Technology at the DeVry Institute of Technology in Chicago.
After a successful career in the electronics industry, Dean returned to the family farm in 2004, joining his brother in managing the family's Heritage farm.
Dean has supported local volunteer fire departments throughout the year by donating his unused legislative expenses, totaling more than $10,000.
The election will be held in November.


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Today, we launched a case at the European Court of Human Rights on behalf of the Arctic 30, who spent two months in Russian jail for a peaceful protest to save the Arctic.
The 30 individuals are requesting "just compensation" from the Russian Federation, and importantly, a statement from the independent Court saying that their apprehension in international waters by Russian agents and subsequent detention were unlawful.
The European Court has the power to hold Russia to account for the months of uncertainty the Arctic 30 faced in Russia. While held in detention centres they lived with the fear that they could spend years locked up for a crime they did not commit. The European Court has jurisdiction over matters involving alleged human rights violations committed by Russia. In many cases Russia has been found liable for such violations and ordered to compensate victims. Ultimately, this case aims to ensure Russia lives up to its human rights commitments.
The Arctic 30 were abducted and forcibly detained by armed Russian agents following a peaceful protest against oil drilling in pristine Arctic waters. During the protest, two unmarked inflatables appeared from the Russian Federal Security Service vessel Ladoga, each manned with at least three Russian State agents in balaclavas with weapons. The Russian agents threw ropes at the propellers of the Greenpeace inflatables. The lines hit some of the activists. The agents proceeded to threaten the activists with guns and knives. Several of the Greenpeace inflatables were punctured with knives.
Once the protest ended, the activists, with the exception of the two brave climbers who were apprehended by Russian agents near the platform, returned to the Greenpeace ship, the Arctic Sunrise. The Russian agents' violent response breached their rights to freedom of expression and has a chilling effect on future peaceful protests aimed at protecting the Arctic.
What followed was a gross violation of the right to liberty. The next day, armed agents of the Russian Federal Security Service boarded the Arctic Sunrise from a helicopter and detained the individuals on board. The Arctic Sunrise was in the exclusive economic zone of the Russian Federation in the Pechora Sea and outside of the Russian-declared three nautical miles' exclusion zone around the oil platform, Prirazlomnaya, which was the target of the protest.
While the Greenpeace ship was being towed to a Russian port by the Russian Authorities, the Arctic 30 were detained onboard without charge for more than five days. The Arctic 30 were threatened with weapons if they did not follow the orders of the Russian agents. They were searched and locked in their cabins or other premises on the Arctic Sunrise. All communication devices were taken from them. No movements were possible without the authorisation of the Russian agents. The authorities provided unfounded legal grounds for the detention only after arriving at a Murmansk port. All 30 were charged with piracy.
Their ordeal became even worse. The activists were locked up in some of Russia's most notorious detention facilities for more than two months. This is despite the fact that the head of the Investigative Committee of the Russian Federation issued a ruling half-way through their time behind bars that the ground for detention, piracy, was determined to be an improper charge, and a decision was made to reclassify the crime to hooliganism. The activists remained behind bars for another month, until finally being released on bail. On Christmas Day 2013, the Investigative Committee officials informed the Arctic 30 that their hooliganism charges were dropped as a result of a recently adopted amnesty decree. They were finally free to return home to their families.
Russia's unlawful actions forever changed their lives. During the protest their safety was put at risk. While on board the Arctic Sunrise as it was being towed to a Russian port they were detained without legal grounds and no opportunity to go before a judge. In detention they faced spending a decade or more behind bars for a crime they didn't commit – a crime that sadly Russian authorities even admitted they couldn't possibly have committed.
The Arctic 30 are not criminals. They are peaceful protesters, journalists and environmental human rights defenders. As the saying 'the millstones of Justice turn exceedingly slow, but grind exceedingly fine' goes, we anticipate that ultimately the European Court will order Russia to compensate the 30 and declare that their rights to freedom of expression and liberty were violated by Russia.
Sergey Golubok is a legal representative for the Arctic 30 before the European Court, and Kristin Casper is Legal Counsel for campaigns & actions at Greenpeace International.
(Unregistered) Sun Wu
Cute...if you happen to be at European Court of Human Rights anyways, why don't you adress Syria, Ukraine etc. aswell.
Sun Wu, godfather of the Rainbow Warrior III
1.) why did I, Sun Wu, oppose this stupid action at Prem-something in 2012 already with saying so in commentatory of DOCTOR Naidoo's posts?
2.) who will take responsibility for this multi-million UDS desaster? This 26 year old campainger claimed to be ambitious and impatient, maybe it would be time for a lesson obviously not having been touched at university
3.) Arctic Sunrise? Can I plan with two Greenpeace-ships, or will I have three available when being CEO of GPI soon?
4.) Don't you think in 2014 the European Court of Human Rights has more serious stuff to do but dealing with a bunch of low-profiles having burned their fingers while playing activist with the wrong opponent?
DEAR MR. PRESIDENT, I would like to invite you to join me on an Arctic cruise on Arctic Sunrise...
5.) can you SINK a rainbow
18 March, 2014 at 14:14
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'Lieber ein Ende mit Schrecken als ein Schrecken ohne Ende'
Regarding Greenpeace vs. Russia
You not making it any be...
'Lieber ein Ende mit Schrecken als ein Schrecken ohne Ende'
Regarding Greenpeace vs. Russia
You not making it any better by making the wimp in court trying to get attention on this 'Putin, the bad president'-wave...If you are not getting my point: DEAR MR. PRESIDENT has started a few really nasty things in Syria and now starting in Ukraine...maybe Baltics next...
I told you in 2012 that you are attacking the wrong persons...since you did not listen but prefered to fuck up there is only two possible strategies:
1.) shut up and try to get AS back with promising yourself to do better next time...
2.) attack GAZPROM wherever they enter the Western World (and forget about Arctic Sunrise which would add another 4-5Million USD to the costs of this fuck up - but as I said, lieber ein Ende mit Schrecken als ein Schrecken ohne Ende).
Sun Wu, attacking SKYSAILS and Niels Stolberg since 2007
18 March, 2014 at 14:29
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If you happen to go for 2.) which I would most likely consider:
I need will need three ships for telling P & G to stop deforestation....
If you happen to go for 2.) which I would most likely consider:
I need will need three ships for telling P & G to stop deforestation...smile this was a joke...to attack the USA.
Please start to work on replacement...ask Mr. DIJKSTRA & his PARTNERS for the Dynarigg!!!
Believe me, it is worth a couple more millions.
Sun Wu, economic engineer of shipping
PS: have I told the Indian in 2008 while having lunch with him at Ottho Heldringstraat that SKYSAILS is a media-set up in order to finance ships?
18 March, 2014 at 14:37
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Save the Arctic...
Sun Wu economic engineer of Shipping
PS: I love India, I will work on my hinduism now....
Save the Arctic...
Sun Wu economic engineer of Shipping
PS: I love India, I will work on my hinduism now....
When I am ready for believing I will be reincarnated Indian but not German.
I got this dream of being Indian and financed by the Germans...a dream worth dreaming.
18 March, 2014 at 14:53
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text: ok, here we go. most have seen this bike already. i'll post what i started out with an what i first built. so i am going to tear it down again an do a redo on it. i really liked it before but there is always a better way. so here are the pic's. i will post pics as i go along so you can see i am really re doing it/the bike is a Murry but i don' know the yr or make. so lets have fun building these make it simple, make it wild, but have fun. Outlaw 8)


text:
by Jordan
DIY Edward Scissorhands Costume Photo 5 of 5
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edward scissorhands with schredded nightmare!!
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This homemade costume for women entered our 2012 Halloween Costume Contest.
A word from Eugenia, the 'Edward Scissorhands' costume creator:
I'm wearing the edward scissorhands costume. I put it together myself. I got the idea about 3 years ago from watching the movie. I'm a big fan of Tim burton and found the costume to... Read more »
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text:
Hello everyone. I am beginer in Java programming. Current chapter i am reading covers if,else and switch. I am doing a lot of hands on and as i read chapters i try to create diffrent codes. Sorry this is probably very simple for you guys but i cant figure it out. i already created similair project just using if but i wanted to do switch one.
Thank you