[226234] in SIPB-AFS-requests
Your Endurance Auto Warranty Offer - $300 off any new policy
daemon@ATHENA.MIT.EDU (Endurance Affiliates)
Thu Feb 6 08:07:07 2025
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Date: Thu, 6 Feb 2025 14:06:35 +0100
From: "Endurance Affiliates" <AutoWarranty@christmasprayer.sa.com>
Reply-To: "Endurance Partners" <AutoWarranty@christmasprayer.sa.com>
Subject: Your Endurance Auto Warranty Offer - $300 off any new policy
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Your Endurance Auto Warranty Offer - $300 off any new policy
http://christmasprayer.sa.com/PjWqnbfjciHESsMwmcVhMmnQakeFZY4ix_eaGD78_HIpVBoSZw
http://christmasprayer.sa.com/k0w2Uz50Rr3FOizhfN7LnD3X-lM0b3DS_KswRA86BHa2twOKSg
at Barrier Reef. Others are found in the deep ocean surrounding islands or as atolls, such as in the Maldives. The reefs surrounding islands form when islands subside into the ocean, and atolls form when an island subsides below the surface of the sea.
Alternatively, Moyle and Cech distinguish six zones, though most reefs possess only some of the zones.
Water in the reef surface zone is often agitated. This diagram represents a reef on a continental shelf. The water waves at the left travel over the off-reef floor until they encounter the reef slope or fore reef. Then the waves pass over the shallow reef crest. When a wave enters shallow water it shoals, that is, it slows down and the wave height increases.
The reef surface is the shallowest part of the reef. It is subject to surge and tides. When waves pass over shallow areas, they shoal, as shown in the adjacent diagram. This means the water is often agitated. These are the precise condition under which corals flourish. The light is sufficient for photosynthesis by the symbiotic zooxanthellae, and agitated water brings plankton to feed the coral.
The off-reef floor is the shallow sea floor surrounding a reef. This zone occurs next to reefs on continental shelves. Reefs around tropical islands and atolls drop abruptly to great depths and do not have such a floor. Usually sandy, the floor often supports seagrass meadows which are important foraging ar
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<div style="color:#FFFFFF;font-size:8px;visibility:hidden;">at Barrier Reef. Others are found in the deep ocean surrounding islands or as atolls, such as in the Maldives. The reefs surrounding islands form when islands subside into the ocean, and atolls form when an island subsides below the surface of the sea. Alternatively, Moyle and Cech distinguish six zones, though most reefs possess only some of the zones. Water in the reef surface zone is often agitated. This diagram represents a reef on a continental shelf. The water waves at the left travel over the off-reef floor until they encounter the reef slope or fore reef. Then the waves pass over the shallow reef crest. When a wave enters shallow water it shoals, that is, it slows down and the wave height increases. The reef surface is the shallowest part of the reef. It is subject to surge and tides. When waves pass over shallow areas, they shoal, as shown in the adjacent diagram. This means the water is often agitated. These are the precise condition under which corals flourish. The light is sufficient for photosynthesis by the symbiotic zooxanthellae, and agitated water brings plankton to feed the coral. The off-reef floor is the shallow sea floor surrounding a reef. This zone occurs next to reefs on continental shelves. Reefs around tropical islands and atolls drop abruptly to great depths and do not have such a floor. Usually sandy, the floor often supports seagrass meadows which are important foraging ar</div>
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