{"id":593,"date":"2019-01-22T15:54:59","date_gmt":"2019-01-22T15:54:59","guid":{"rendered":"http:\/\/www.geology.unibe.ch\/wp\/?p=593"},"modified":"2019-01-22T15:56:24","modified_gmt":"2019-01-22T15:56:24","slug":"tracking-the-pace-of-the-pliocene-and-last-interglacial-warmings","status":"publish","type":"post","link":"https:\/\/www.geology.unibe.ch\/index.php\/2019\/01\/22\/tracking-the-pace-of-the-pliocene-and-last-interglacial-warmings\/","title":{"rendered":"Tracking the pace of the Pliocene and Last Interglacial warmings"},"content":{"rendered":"

DEAIS @ Mount Nils Larsen: Tracking the pace of the Pliocene and Last Interglacial warmings<\/strong><\/p>\n

(report from PD Dr. Naki Ak\u00e7ar<\/a>, Institute of Geological Sciences, University of Bern)<\/p>\n

Recent ice sheet reconstructions and climate models indicate that the polar temperatures and global mean sea level were slightly higher than today at least two times: during the Last Interglacial (LIG; 130,000 to 115,000 years ago) and the Pliocene. Although a dramatic surface lowering of East Antarctic Ice Sheet (EAIS) during the last million years have been recently reported, the spatial distribution of this lowering, especially in response to the LIG and Pliocene warmings, remains unexplored. In order to discover EAIS\u2019 behavior during the two times of slightly warmer climate, we focus on the S\u00f8r Rondane Mountains in the Queen Maud Land, which acts as a barrier to the EAIS. This is displayed by the difference in altitude of the ice surface to the south and north of the mountain chain. To the south, ice surface reaches altitudes above 2500 meters above sea level. Lowlands of ice are found at altitudes of around 1500 meters to the north of the mountain chain. Such an ice-landscape makes the S\u00f8r Rondane Mountains an ideal field laboratory to track the pace of the LIG and Pliocene warmings. <\/span><\/p>\n

Based on our results of the BELARE 2017-2018 Expedition, we suggest that the surface of the EAIS during the late Miocene was at least 400 meters higher than today and thus the ice from the plateau was drained towards northeast over the mountain range. At the beginning of Pliocene, ice surface started to decrease and the south-north linkage was already broken prior to the Early Pleistocene. This surface lowering caused the ice drainage to be channelized into either across or around the mountain range. Afterwards, a second dramatic decrease in the ice surface elevation occurred during the LIG, in contrast to the Pliocene lowering, this decrease seems to be limited to the ice lowlands to the north of the mountain chain and the ice plateau to the south were not affected by the dramatic changes occurred on the northern side of the mountain range.<\/span><\/p>\n

\"Mount<\/a>

Glacial deposits on the western part of Mount Nils Larsen. View towards west<\/p><\/div>\n

During this austral summer 2018-2019, we focused on the tills deposited by the Hansen Glacier, which are located few hundred meters above today\u2019s ice surface at Mount Nils Larsen in the southwest S\u00f8r Rondane Mountains. These deposits cover the metamorphic bedrock rock and are their thickness locally reaches more than 100 meters. In the past, the Hansen Glacier built a succession of right lateral moraines on the western side of the mountain.  <\/span><\/p>\n

On January 3rd<\/sup>, me, Dr. Mehmet Ye<\/span>\u015filta<\/span>\u015f (Meteorite Researcher from Turkey) and Manu Poudelet (our guide) left the Princess Elisabeth Antarctica Station with three snow mobiles and three sledges. After 3 hours of drive along 50 km, we arrived to our camp site at Nils Larsen, where we installed one kitchen, one toilet and three sleeping tents. Until January 8th<\/sup>, Dr. Ye\u015filta\u015f and our guide went to the plateau and hunted for meteorites, while I, for the first time in my life, worked alone in the field. After Dr. Ye\u015filta\u015f completed his search and returned to the station, our guide had accompanied me in the field. <\/span><\/p>\n

\"Sampled<\/a>

Sampled erratic boulder along the crest of one of the right lateral moraines of the Hansen Glacier.<\/p><\/div>\n

I focused on the succession of right lateral moraines. I identified 35 erratic boulders along the crest of these and sampled their top most surfaces for cosmogenic nuclide analysis. After, I completed the sampling, I started with flight missions of the unmanned aerial vehicle in order to reconstruct high resolution digital elevation model of the study area. On January 10th<\/sup>, during one of the flight missions, the connection to the drone was broken and we lost the drone. After around five hours, we found it. It was almost undamaged, only one propeller was broken. As a snow storm started early Friday morning January 10th<\/sup>, we decided to go back to the station. Snow storm continued until early Monday morning. On Monday January 14th<\/sup>, we went back to Mount Nils Larsen to accomplish the remaining flight missions.<\/span><\/p>\n

This year we were lucky and we had around 10 days of good weather for camping. We successfully completed our field campaign at Nils Larsen. Now, I\u2019m preparing reconnaissance fieldtrips to other mountains located at the south and east of the chain, such as Duffekfjellet and Norhaugen. We continue tracing the pace of past warming phases and their geo-archives. <\/span><\/p>\n

\"Our<\/a>

Our camp at Nils Larsen<\/p><\/div>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

DEAIS @ Mount Nils Larsen: Tracking the pace of the Pliocene and Last Interglacial warmings (report from PD Dr. Naki Ak\u00e7ar, Institute of Geological Sciences, University of Bern) Recent ice sheet reconstructions and climate models Read more…<\/a><\/p>\n","protected":false},"author":2,"featured_media":595,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0},"categories":[5],"tags":[9],"_links":{"self":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/593"}],"collection":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/comments?post=593"}],"version-history":[{"count":2,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/593\/revisions"}],"predecessor-version":[{"id":598,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/posts\/593\/revisions\/598"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/media\/595"}],"wp:attachment":[{"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/media?parent=593"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/categories?post=593"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.geology.unibe.ch\/index.php\/wp-json\/wp\/v2\/tags?post=593"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}