Thursday, May 29, 2014

# 10 - Cape Roberts

I realized I forgot to include my video from last time, so here it is: https://www.youtube.com/watch?v=TvkZFIRR-bc
Be sure to turn up the quality so you can get the full experience. It includes highlights from the entire trip. 

Cape Roberts: Life on the Coast 

While we focused on the coast during our field season last year, we decided to come back to spots we weren't able to visit during that season, Cape Roberts, Marble and Gneiss Points. Cape Roberts was full of all kinds of wildlife as an active Skua nesting ground with plenty of Weddell seals nearby on the sea ice. 


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Left - A view of the sea ice with Taylor Valley and Explorer's Cove in the background, sites we covered in the 2012-2013 field season on the way to Cape Roberts. Right - Wilson Piedmont and Spike Cape, on the way to Cape Roberts. The Piedmont has been shrinking back over the past several decades, exposing mummies that had been long buried under ice.

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Left - A Skua pair at Cape Roberts, claiming their territory and challenging anything that comes near it. Right - A Skua mother and chick, with the mother doing her thing, calling out to make us aware of her presence. 

For those unfamiliar with the term "Skua," I'll introduce them to you as fat devil birds. The South Polar Skuas (Skoo-uh) are highly territorial, aggressive, scavenging sea birds that nest on the Antarctic coast during the summer and migrate throughout the entire world during the winter. Skuas are territorial and aggressive for a good reason: these birds are cannibals. They'll eat each others young when given the opportunity. For example, in desperate times, a Skua will distract a mother away from her chick, and the other member of the hunting Skua pair will dive in and grab the chick while it's trying to hide under a rock. Skuas will also fight to the death over drinking water ponds, as evidenced by the clearly scavenged Skua bodies we found nearby. 


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Left - A Weddell seal lying out on the sea ice near a big crack in the ice. The bottom of Mt. Erebus lies in the background just to the right of a large iceberg. Right - A recently deceased Weddell Seal is being scavenged by Skuas. 

The only other animals nearby are Weddell Seals, which typically lie out on the sea ice near accessible diving spots. Unlike other seals in Antarctica, Weddell's prefer to lay out on the ice all the time, whereas Crabeater seals will venture out into the open ocean during the summer, with Leopard Seals following (and hunting) the Crabeaters. Weddell seals will either take advantage of naturally formed cracks in the ice, or use their teeth to break through so they can go fishing below. Weddell's were one of the three main species of seals we were looking for. Judging by Weddell carcasses we found on the coast, Skuas had a hard time scavenging carcasses in areas other than the eyes or perhaps they just really like eyes. So if you fall asleep along the coast, you might want to be careful about your eyes. 

Southern Elephant Seals prefer north facing beaches and open water. In the project that inspired this one, Elephant Seals were the main focus since they have a complicated history on the Antarctic coast, and especially the Ross Sea. Several thousand years ago, when the Ross Sea had more open water, The largest known Elephant Seal colony existed in the Ross Sea. Around 1000 years ago, a regional cooling trend froze the Ross Sea, and the local Elephant Seal population collapsed, leaving behind only traces of fur that can be found on ancient beaches under rocks. Though we were searching for other species of seals in the main focus of the project, we were also looking for Elephant Seal fur that was left behind to find out more about ancient Elephant Seal populations as a small side project. Now that the Ross Sea is warming back up, we want to find out how other seal species will react to this climate change, and if the Elephant seals might return to these formerly populated beaches.

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Left - Skuas defending territory on the rocks at Cape Roberts. Right - A weather station at Cape Roberts. 

And that's about it for this email. I had a few questions since the last one, mostly about the timing of events and seal evolution. In terms of the sequence of Geologic events, Antarctica was not centered on the South Pole like it is today in the Mesozoic. At the time, Dinosaurs, trees and productive ecosystems existed with fossils of both in the sediments of the Royal Society Range (near Marshall Valley). The Ross Sea formed as a rift system, leading to volcanic activity that is still present with Mt. Erebus. As Antarctica centered over the South Pole in the Paleogene, the Southern Ocean formed a circular current which increased the cooling effect around the continent, which not only drove temperatures down around the continent, but around the entire world, killing off normal life in Antarctica. Significant amounts of ice and glacier penetrated into the valleys and receded repeatedly beginning in the Miocene until the Last Glacial Maximum in the Pleistocene. The first known seals are known from temperate environments, including California, in the Oligocene and Miocene. The three major groups of seals didn't separate until later on in the Pliocene. The five species of Antarctic seals are the Southern Elephant Seal (beach loving seals with colonies), Crabeater Seals (the most abundant seal, and possibly the most abundant large mammal after humans on Earth), Weddell Seals (sea ice lovers), and the rare and elusive Ross Seal (rare, elusive, deep divers out in the open ocean). 

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That was a quick and dirty summary of the background. If something doesn't make any sense let me know!

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