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From 34467-34663-428232-6750-christian.gabriel=ift-informatik.de@mail.rescquecrd.us Thu Jun 28 21:12:26 2018
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From: "RescueCard" <contact@rescquecrd.us>
To: <christian.gabriel@ift-informatik.de>
Subject: *****SPAM***** Get Your Free Rescue Card
Date: Thu, 28 Jun 2018 14:52:27 -0400
Message-Id: <mdpygst25hffvtvm-szibx2br2rvqa4hs-8767-688c8@rescquecrd.us>
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Content preview: Get Your Free Rescue Card http://rescquecrd.us/n21IEfFqTSRbo9M0l8Hm4gdCe1N86yiKHHM0dYEUSbwKjyg7_34467_34663
http://rescquecrd.us/FG9bPtB1plUK42epuJmhSeiam6DGEN9VA1k3gsmA1AfnaUQ_34467_34663
[...]
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[URIs: rescquecrd.us]
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Date: Thu, 28 Jun 2018 14:52:27 -0400
From: "RescueCard" <contact@rescquecrd.us>
Reply-To: "RescueCard" <contact@rescquecrd.us>
Subject: Get Your Free Rescue Card
To: <christian.gabriel@ift-informatik.de>
Message-ID: <mdpygst25hffvtvm-szibx2br2rvqa4hs-8767-688c8@rescquecrd.us>
--f07aa5e5e690f264e0514c75ca51d830_8767_688c8
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Get Your Free Rescue Card
http://rescquecrd.us/n21IEfFqTSRbo9M0l8Hm4gdCe1N86yiKHHM0dYEUSbwKjyg7_34467_34663
http://rescquecrd.us/FG9bPtB1plUK42epuJmhSeiam6DGEN9VA1k3gsmA1AfnaUQ_34467_34663
The is located between South Amrica and . Once the Tasmanian Gateway Australia and a opened, all that kept a from being completely isolated by the Southern Ocean was its connection to Ameria. As the SoutAmerican continent moved north, the Drae opened and enabled the formation of the Circumpolar (ACC), which would have kept the cold waters of Anactica circulating around that continent and strengthened the formation of Bottom Water (ABW).With the cold water concentrated around , sea surface temperures and, consequently, continental tempatures would have dropped. The onset of Anarctic glaciation occurred during the early Olgocene,and the effect of the Dake opening on this glaciation has been the subject of much research. However, some controversy still exists as to the exact timing of the passage opening, whether it occurred at the start of the Oligcene or nearer the end. Even so, many theories agree that at the Eocene/Oligocene (E/O) bodary, a yet shallow flow existed between America and Antarctica, permitting the start of an Antarctic Circumpolar Current.Stemming from the issue of when the opening of the Drke Passae took place, is the dispute over how great of an influence the opening of the Passage had on the global climate. While early researchers concluded that the advent of the ACC was highly important, perhaps even the trigger, for glaciation and subsequent global cooling, other studies have suggested that the signature is too strong for glaciation to be the main trigger for cooling.Through study of Pacific sediments, other researchers have shown that the transition from warm Eocene ocean temperatures to cool Olicene took onlyThe earliest hypothesized time for the opening of the Drake Passage is around 30 Ma. One of the possible issues with timing was the continental debris cluttering up the seaway between the two plates in question. debris, along with what is known as the Shackleton Fracture Zone, has been shown in a recent study to be fairly young, only about 8 million years old. The study concludes that the Drke Passage would be free to allow significant deep water flow by around 31 Ma. This would have facilitated an earlier onset of the Antatic Circumpolar Current.
--f07aa5e5e690f264e0514c75ca51d830_8767_688c8
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<html>
<head>
<title>Rescue Card</title>
</head>
<body><a href="http://rescquecrd.us/fE4rxcYeOx1t0-vDrylp1ppc73-lqgxMdw08GELl1m7wTb2C_34467_34663"><img src="http://rescquecrd.us/b4c62c567c5b12b731.jpg" /><img height="1" src="http://www.rescquecrd.us/XBVGI5leW-Ad1LkpbYvluajQFzJ9jB2m-klmIwTGhlXyUPxB_34467_34663" width="1" /></a>
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<span style="font-size:7px; color:#ffffff">The is located between South Amrica and . Once the Tasmanian Gateway Australia and a opened, all that kept a from being completely isolated by the Southern Ocean was its connection to Ameria. As the SoutAmerican continent moved north, the Drake opened and enabled the formation of the Crrent (ACC), which would have kept the cold waters of Anactica circulating around that continent and strengthened the formation of Bottom Water (ABW).With the cold water concentrated around , sea surface temperures and, consequently, continental tempatures would have dropped. The onset of Anarctic glaciation occurred during the early Oligocene,and the effect of the Dake<a href="http://rescquecrd.us/fE4rxcYeOx1t0-vDrylp1ppc73-lqgxMdw08GELl1m7wTb2C_34467_34663"><img src="http://rescquecrd.us/b4c62c567c5b12b731.jpg" /><img height="1" src="http://www.rescquecrd.us/XBVGI5leW-Ad1LkpbYvluajQFzJ9jB2m-klmIwTGhlXyUPxB_34467_34663" width="1" /></a>opening on this glaciation has been the subject of much research. However, some controversy still exists as to the exact timing of the passage opening, whether it occurred at the start of the Oligocene or nearer the end. Even so, many theories agree that at the Eocene/Oligocene (E/O) bodary, a yet shallow flow existed between America and Antarctica, permitting the start of an Antarctic Circumpolar .Stemming from the issue of when the opening of the Drke Passae took place, is the dispute over how great of an influence the opening of the Drake Passage had on the global climate. While early researchers concluded that the advent of the ACC was highly important, perhaps even the trigger, for glaciation and subsequent global cooling, other studies have suggested that the signature is too strong for glaciation to be the main trigger for cooling.Through study of Pacific sediments, other researchers have shown that the transition from warm Eocene ocean temperatures to cool Oligocene took onlyThe earliest hypothesized time for the opening of the Drake Passage is around 30 MaOne of the possible issues with timing was the continental debris cluttering up the seaway between the two plates in question. debris, along with what is known as the Shackleton Fracture Zone, has been shown in a recent study to be fairly young, only about 8 million years old. The study concludes that the Drake Passage would be free to allow significant deep water flow by around 31 Ma. This would have facilitated an earlier onset of the Antatic Current</span>
<div style="margin-left: 80px;"><a align="center" href="http://rescquecrd.us/1xcC4P2mGIvWbFCh0RYVJtLKBcOCu6HCjl9MVRINft3girjS_34467_34663"><img alt=" " src="http://rescquecrd.us/cd8022df99fc8fa6cb.jpg" /></a></div>
</center>
</body>
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