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FatKidWitAJetPak

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FatKidWitAJetPak

Age/Gender: 16, Male
Location: Qrbrbbrlbrll Town
Job: Flipping Flapjacks

Yeah, I like Pancakes... Pancakes, pancakes, pancakes... and muffins. Oh and please listen to some of my music. I always respond to reviews! Thanks. And yes, that picture is me. I have a strange growth syndrome. P.S. Email me for help with Garageband. :)

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7/28/07

Level: 16
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Entry #23

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FatKidWitAJetPak

MUSIC GETTING GOOD. :0

Posted by FatKidWitAJetPak Mar. 9, 2008 @ 1:37 PM EDT

:0 Yes that's right, my music is improving... HURRAI. People are starting to select my music for their games... In fact.. I might just have my song (::Towards The Sun::) in the upcoming game, Gateway III. I hope it gets in there... 0_0 Well anyway, I just realized that my song (::Lucky 7::) GWC is featured in 25 games right now... LOL. That is exactly why so many people are 0 bombing it. XD Well feel free to review some of my stuff if you want. I always respond, and would be happy to review yours.

OK WHAT THE HECK?!!? I HAVE THESE TWO ON THE TOP... BUT THEY NEVER GOT TOP OF THE WEEK. >:(

ROOOOAAAARRRRRW!!!!

Yeah, I cam out with another song so erm... ENJOY! ^____^

Picture_1.jpg

Updated: 03/13/08 10:07 PM Log in to comment! | Share this!

The People Have Spoken

13 Comments

Mar. 9, 2008 | 6:50 PM straightpimpin1 says:

thats awesome ive been supporting all your music!

Mar. 9, 2008 | 9:34 PM FatKidWitAJetPak responds:

THANKS!!!


Mar. 9, 2008 | 11:21 PM TAUfanatic says:

sounds.......relaxing.........I LIKE IT!!!!! ( and maybe not "fairly skinny"........she is

Mar. 10, 2008 | 8:03 AM FatKidWitAJetPak responds:

Oh, we are still having that conversation? Lol.


Mar. 10, 2008 | 5:53 PM ricksed says:

Your improving at an increably high rate.

Mar. 10, 2008 | 5:55 PM FatKidWitAJetPak responds:

Really? WELL THANKS! ^_^


Mar. 10, 2008 | 6:37 PM Suspended-3rd-Chord says:

well, congrats

Mar. 10, 2008 | 9:02 PM FatKidWitAJetPak responds:

THanks!


Mar. 11, 2008 | 8:28 PM Sparkwattclock says:

hey man!!!!

Mar. 11, 2008 | 11:03 PM FatKidWitAJetPak responds:

SUP.


Mar. 11, 2008 | 10:11 PM TAUfanatic says:

idk,I had to respond to your response,although I'm done now,but yeah,your music is good

Mar. 11, 2008 | 11:03 PM FatKidWitAJetPak responds:

Thanks lol.


Mar. 13, 2008 | 12:15 AM flashmac says:

You still use garageband?

Mar. 13, 2008 | 6:10 PM FatKidWitAJetPak responds:

You bet I do. I have learned a lot. Like how to make my own loops, sounds, filters, e.t.c. :)


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Mar. 13, 2008 | 6:12 PM FatKidWitAJetPak responds:

here is variability in the fossil record as to the extinction rate of marine invertebrates across the K-T boundary. The apparent rate is influenced by the lack of fossil records rather than actual extinction.[7]
Ostracodes, a class of small crustaceans that were prevalent in the upper Maastrichtian, left fossil deposits in a variety of locations. A review of these fossils shows that ostracode diversity was lower in the Paleocene than any other time in the Tertiary. However, current research cannot ascertain whether the extinctions occurred prior to or during the boundary interval itself.[25][26]
Approximately 60% of late-Cretaceous Scleractinia coral genera failed to cross the K-T boundary into the Paleocene. Further analysis of the coral extinctions show that approximately 98% of colonial species, ones that inhabit warm, shallow tropical waters, went extinct. The solitary corals, which generally do not form reefs and inhabit colder and deeper (below the photic zone) areas of the ocean were less impacted by the K-T boundary. Colonial coral species rely upon symbiosis with photosynthetic algae, which collapsed due to the events surrounding the K-T boundary.[27][28] However, the use of data from coral fossils to support K-T extinction and subsequent Paleocene recovery must be weighed against the changes that occurred in coral ecosystems through the K-T boundary.[7]
The numbers of cephalopod, echinoderm, and bivalve genera exhibited significant diminution after the K-T boundary.[7] Most species of brachiopods, a small phylum of marine invertebrates, survived the K-T event and diversified during the early Paleocene.
Except for nautiloids (represented by the modern order Nautilida) and coleoids (which had already diverged into modern octopi, squids, and cuttlefish) all other species of the molluscan class Cephalopoda went extinct at the K-T boundary. These included the ecologically significant belemnoids, as well as the ammonoids, a group of highly diverse, numerous, and widely distributed shelled cephalopods. Researchers have pointed out that the reproductive strategy of the surviving nautiloids, which rely upon few and larger eggs, played a role in outsurviving their ammonoid counterparts through the extinction event. The ammonoids utilized a planktonic strategy of reproduction (numerous eggs and planktonic larvae), which would have been devastated by the K-T boundary event. Additional research has shown that subsequent to this elimination of ammonoids from the global biota, nautiloids began an evolutionary radiation into shell shapes and complexities theretofore known only from ammonoids.[29][30]
Approximately 35% of echinoderm genera went extinct at the K-T boundary, although taxa that thrived in low-latitude, shallow-water environments during late Cretaceous had the highest extinction rate. Mid-latitude, deep-water echinoderms were much less affected at the K-T boundary. The pattern of extinction points to habitat loss, specifically the drowning of carbonate platforms, the shallow-water reefs in existence at that time, by the extinction event.[31]
Other invertebrate groups, including rudists (reef-building clams) and inoceramids (giant relatives of modern scallops), also became completely extinct at the K-T boundary.[32][33]
[edit]Fish

Apparent fraction of marine animal genera going extinct at any given time, as reconstructed from the fossil record.
There are substantial fossil records of jawed fishes across the K-T boundary, which provides good evidence of extinction patterns of these classes of marine vertebrates. Within cartilaginous fish, approximately 80% of the sharks, rays, and skates families survived the extinction event,[7] and fewer than 10% of teleost fish (bony fish) families became extinct.[34] There is evidence of a mass kill of bony fishes at a fossil site immediately above the K-T boundary layer on Seymour Island near Antarctica. It is speculated that fish were undergoing environmental stresses and the K-T boundary event may have precipitated the mass extinction.[35] However, the marine and freshwater environments of fishes mitigated environmental effects of the extinction event.[36]
[edit]Terrestrial invertebrates
Insect damage to the fossilized leaves of flowering plants from fourteen sites in North America were used as a proxy for insect diversity across the K-T boundary and analyzed to determine the rate of extinction. Researchers found that Cretaceous sites, prior to the extinction event, had rich plant and insect-feeding diversity. However, during the early Paleocene, flora were relatively diverse with little predation from insects, even 1.7 million years after the extinction event.[37][38]
[edit]Terrestrial plants
There is overwhelming evidence of global disruption of plant communities at the K-T boundary.[39] However, there were important regional differences in plant succession. In North America, the data suggest massive devastation and mass extinction of plants at the K-T boundary sections, although there were substantial megafloral changes before the boundary.[40]
In high southern hemisphere latitudes, such as New Zealand and Antarctica the mass die-off of flora caused no significant turnover in species, but dramatic and short-term changes in the relative abundance of plant groups.[41][37] In North America, approximately 57% of plant species became extinct. The Paleocene recovery of plants began with recolonizations by fern species, represented as a fern spike in the geologic record; this same type of fern recolonization was observed after the 1980 Mount St. Helens eruption.[42]
Due to the wholesale destruction of plants at the K-T boundary, there was a significant proliferation of saprophytic organisms such as fungi which do not require photosynthesis and utilize nutrients from of decaying vegetation. The dominance of fungal species lasted only a few years while the atmosphere cleared and there was plenty of organic matter to feed on. Once the atmosphere cleared, photosynthetic organisms like ferns and other plants returned.[43]
[edit]Amphibians
There is no evidence of K-T boundary mass extinctions of amphibians, and there is strong evidence that most amphibians survived the event relatively unscathed.[7] Several in-depth studies of salamander genera in fossil beds in Montana show that six of seven genera were unchanged after the event.[44]
Frog species appear to have survived into the Paleocene with few species becoming extinct. However, the fossil record for frog families and genera is uneven.[7] An extensive survey of three genera of frogs in Montana show that they were unaffected by the K-T event and survived apparently unchanged.[44] The data show little or no evidence for extinction of amphibian families that bracket the K-T event. Amphibian survival resulted from the clade's ability to seek shelter in water or to build burrows in sediments, soil, wood, or beneath rocks.[36]
[edit]Non-archosaur reptiles
The two living non-archosaurian reptile taxa, testudines (turtles) and lepidosaurs (snakes, lizards, and worm lizards), along with champsosaurs (semi-aquatic archosauromorphs which died out in the early Miocene), survived through the K-T boundary.[7] Over 80% of Cretaceous turtle species passed through the K-T boundary. Additionally, all six turtle families in existence at the end of the Cretaceous survived into the Tertiary and are represented by current species.[45]
Living lepidosaurs include Rhynchocephalia and Squamata. The Rhynchocephalia, or tuatara, were a widespread and relatively successful group of lepidosaurs in the early Mesozoic, but began to decline by the mid-Cretaceous. They are represented today by a single genus located exclusively in New Zealand.[46]
The order Squamata, which is represented today by lizards, snakes, and amphisbaenia, radiated into various ecological niches during the Jurassic and were successful throughout the Cretaceous. They survived through the K-T boundary and are currently the most successful and diverse group of living reptiles with more than 6,000 extant species.

SO as you can clearly see, ASHJD98GHW958HYQGAHJF8Q5HQ838Q3HY 5FGHAIRHQ085GHQ850QYEIUFHGIAH0H50 8.


Mar. 14, 2008 | 4:21 AM Tivaelydoc says:

Touche!

Mar. 14, 2008 | 12:56 PM FatKidWitAJetPak responds:

Lol.


Mar. 15, 2008 | 6:25 PM loogiesquared says:

hayy.

Mar. 16, 2008 | 3:40 AM FatKidWitAJetPak responds:

HAI THERE.


Mar. 16, 2008 | 3:07 PM loogiesquared says:

i don't really like gateway as a game.

Mar. 16, 2008 | 5:59 PM FatKidWitAJetPak responds:

I like it because it brought ters to my eyes... *sniff*

Lol.


Mar. 16, 2008 | 5:59 PM FatKidWitAJetPak responds:

change that 4.53 to a 4.60 and you got it. :D

THANKS!!!


Mar. 17, 2008 | 11:59 AM loogiesquared says:

VA gettin' good too

multi-program audio collab?

http://i164.photobucket.com/albums/u3 2/213932/8-1.jpg

Mar. 17, 2008 | 1:20 PM FatKidWitAJetPak responds:

LOL, sure why not. ^__________^

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