LAC wrap up meeting

The NERC-funded Lakes and the Arctic Carbon Cycle (LAC) project draws to a close this month and so the team met in the New Forest to work on finalising the datasets and paper writing. The focus of this meeting was interpreting the Holocene sediment record from Ruppert Lake in Alaska. The extensive suite of proxies analysed on this sediment core includes pollen and plant macrofossils to detect shifts in terrestrial vegetation and remains produced within the lake including geochemical elements, stable isotopes analysed on the organic fraction of sediment, chlorophyll and carotenoid pigments and diatoms. The results arising from the project indicate that terrestrial vegetation shifts have a clear effect on the structure and function of lake ecosystems, indicating that Arctic “greening” has the potential to substantially modify net carbon fluxes between the lake and catchment, with implications of for terrestrial carbon budgets on the landscape scale.P1010449

LAC project members attend conferences in Japan and China

We presented research from the LAC project and from Disko Island at two conferences in Asia this summer. The INQUA conference in Japan (26th July to 2nd August) was held in Nagoya and is held every four years for researchers who study the Quaternary time period (divided into the Pleistocene and Holocene). Suzanne McGowan presented her pigment results from multiple Arctic lakes in northern Norway, Alaska and Greenland, while Pete Langdon presented a poster on the LAC project as well as convening a special session on ‘Tipping points in the late Quaternary’. Mark Stevenson presented his PhD research on Arctic Lakes in Disko Island, west Greenland which included pigment and carbon isotope results. Everyone who attended was in agreement that the INQUA congress was very comprehensive and a great opportunity to networking. Highlighting the importance of this conference to Japan, the emperor and empress of Japan were in attendance at the opening ceremony!

We then made the 3,000km journey (two or three consecutive flights) to Lanzhou in the central interior of China. Here we attended the IPS (International Paleolimnology Symposium) at Lanzhou, China (4th to 7th August). The hospitality offered by the organising committee was very generous and the conference was again a great place to network. We were joined by Maarten van Hardenbroek who gave an excellent presentation on the Alaskan elements of the LAC project and John Anderson who convened a session and spoke enthusiastically on Nitrogen dynamics, which included many references to carbon cycling. The audience were impressed by the detail of the changes that linked to the tree-line advance. Suzanne McGowan in her keynote outlined the importance of ‘ecology’ within palaeo reconstructions, and Mark Stevenson gave his talk on carbon cycling in Disko Island lakes to the west of Greenland. Pete Langdon presented the LAC poster which sparked many hours of discussion and debate and presented an enthusiastic talk on using salmon populations to reconstruct changes in the Atlantic over the past 2,000 years.

We really enjoyed the conferences and are now going into the final stages of the project. As the data rolls in our understanding of the importance of Arctic lakes in the global carbon cycle increases!

 

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Suzanne McGowan at INQUA presenting on carbon cycling using pigments in Arctic lake sediments

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Pete Langdon at INQUA presenting the LAC poster

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Silhouette of Mark Stevenson at IPS presenting on reconstructing carbon cycling using Dikso Island lake sediments, West Greenland

Lipid biomarkers at Newcastle University

Earlier in December I spent some time at Newcastle University continuing the lipid biomarker analysis, which is part of my project. Lipid biomarker analysis should allow me to gain more information about terrestrial (land), aquatic (in-lake) and microbial changes in the sediment cores from Disko Island, West Greenland.

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Here I am next to the microwave digester which heats the sediments up in solvents to extract the lipids.

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This photograph displays the finished ‘acid’ extracts and the drying down cabinet used to evaporate solvents and leave only the extracts in the test tubes.

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I’m pleased the labwork earlier in December went so well and plan to return to Newcastle to complete the procedure next week.

Happy New Year,

Mark

Laksebugt (Salmon Bay) lake

After returning from Blæsedalen we had a couple of days of cloudy damp weather so we used the time to explore the local area and recover from mosquito bites, waiting for the weather to improve.

A grey day, but we did manage to spot a whale so it turned out rather well!

A grey day, but we did manage to spot a whale so it turned out rather well!

Through the fog and mist we managed to spot a Fin whale in the Disko Bay near the Arktisk Station.  Fin whale, the second largest whale species, are an endangered species, so it was an amazing sight.

Mark could not resist picking up a lump of iceberg!

Mark could not resist picking up a lump of iceberg!

We walked along the black basalt beach which is so dark as the upper layers of rocks on Dikso Island are primarily volcanic.  Mark could not resist picking up a lump of iceberg!  This ice will have likely been deposited as snow possibly hundreds, or even thousands of years on the Greenland ice sheet.  It most probably entered the sea in the Ilulissat Ice fjord 100km to the East of Disko Bay.

Arktisk Stations research vessel Porsild within the Qeqertarsuaq harbour.

Arktisk Stations research vessel Porsild within the Qeqertarsuaq harbour.

Image of the stations research vessel Porsild in the Qeqertarsuaq harbour.   The weather cleared up on Wednesday and the rough sea became much calmer so with the station logistics leader Akaaraq we went by speed boat west around the coast to the bay Laksebugt.

An iceberg beached by the coast in contrast to the dark blue sea and the basaltic cliffs.

An iceberg beached by the coast in contrast to the dark blue sea and the basaltic cliffs.

Tim, Akaaraq and Mark on the speedboat to Lakesebugt (Salmon Bay)

Tim, Akaaraq and Mark on the speedboat to Lakesebugt (Salmon Bay)

Akaaraq heading off after dropping us off on the beach

Akaaraq heading off after dropping us off on the beach

The journey was very exciting and fast with such a powerful speedboat.  We saw many ice burgs and were joined by Tim from Durham University and Kathryn who is based at Queen Mary in the University of London.  When I was here in April Tim and Kathryn were also visiting Artksik station so it is amazing that they have chosen to return at the same time.  Tim and Kathryn are researching the seasonal variations in Glacial Geomorphology here on Disko Island.  You can find out more about their work here.

Arrival at Disko 4 as the cloud begins to evaporate.

Arrival at Disko 4 as the cloud begins to evaporate.

Image of the sampling site at lake Disko 4

Image of the sampling site at lake Disko 4

Mark in his mosquito net at Disko 4

Mark in his mosquito net at Disko 4

A panoramic shot of Disko 4 after the sun came out a short time after starting the fieldwork.

A panoramic shot of Disko 4 after the sun came out a short time after starting the fieldwork.

We reached Laksebugt after about 45 minutes on the boat and promptly set off for the lake, which is at about 350m above sea level through quite boggy terrain. It was well worth the hike though, because, despite the persistent mosquitos, the lake was beautiful and we were lucky enough to have blue skies for much of the day. The fieldwork went well and all samples were collected without incident over the course of around 5 hours before we began the hike by down to the beach. The views on the decent were fantastic (see below).

A spectacular view of Lakesebugt (salmon) Bay on the way back down to the beach.

A spectacular view of Lakesebugt (salmon) Bay on the way back down to the beach.

The return journey home with the spray from the speedboat as we launched our way back to Qeqertarsuaq harbour.

The return journey home with the spray from the speedboat as we launched our way back to Qeqertarsuaq harbour.

 

Admiring the view on the journey home.

Admiring the view on the journey home.

Icebergs glisten in the sun on the way back to Arctic Station.

Icebergs glisten in the sun on the way back to Arctic Station.

 

Return from lakes Disko 1 and 2

We have returned from four days of fieldwork visiting two lakes in the Blæsedalen valley (in Greenlandic, Itinneq Kangilleq) here on Dikso Island.  The hiking was very tough as the terrain is very hummocky, requiring passage through boulders, cobbles, bog, moss and shrubs while carrying our provisions and field equipment.  To get to our base camp near the first lake took about 9 hours of hiking, but the continuous 24 hour light here in the Arctic meant there was no rush for dusk.100_4253Image of the Blæsedalen valley on the first day.  Low cloud covered the valley, but visibility was sufficient although the peaks of the valley walls could not be seen.

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100_4289The first lake, named Disko 1 for the purposes of this project became visible as the clouds evaporated on the second day.

100_4286The lake is approximately 1km wide and is surrounded by a mossy, guano rich bog. Disko 1 lies in the central part of the Blæsedalen valley at an altitude of approximately 388 meters. An example of the terrain and small ponds surrounding lake Disko 1.

100_4292An attack by mosquitoes at lake Disko 1. Despite covering myself in Jungle Formula DEET, ‘Mosiguard’ and homemade citronella extract repellent I still got no fewer than 15 bites. Joe was not on the mosquitoes menu and only got a couple of bites!

100_4297Water sampling at lake Disko 1.  We took lake water samples for nutrient analysis back in the lab and filtered lake water for lipid and pigment source studies.  We also measured dissolved oxygen, temperature, conductivity and pH using a YSI probe that was calibrated in the field.

100_4315On the third day we hiked for about three hours to lake Disko 2 which lies in a glacially scoured basin with steep head walls at either side.  Here, at an altitude of 630 meters the vegetation is sparse and the soil is poorly developed in many places.   Freeze-thawing is a key action responsible for weathering the basaltic cliffs and is responsible for mounds boulders surrounding the lake.

100_4317After the limnology was completed we took soil and plant samples from the surrounding catchment and estimated plant coverage using quadrats at sites in a transect from the lake basin.  We decided due to the terrain that it was better to return to our base near Disko 1 to spend the night.

100_4329The hut where we stayed for three nights, located in the Blæsedalen valley about 45 mins walk from lake Disko 1.

100_4332The view of the Blæsedalen valley as we embarked on the hike back to Arktisk Station.

100_4380Arktisk Station comes into view as we return after four days fieldwork.

We are now rested after a day to catch up on sleep and have eaten lots of Greenlandic produce to boost our energy levels.  Tomorrow we will take a motor boat sailed by Akaaraq in a westerly direction around the coast from Qeqertarsuaq to a beach at Laksebugt (Itilleq) from where we will hike across Iparaatsi to lake Disko 4 and repeat our water sampling and vegetation surveys.

Arrival at Disko

From Ilulissat, we boarded the Disko Line ferry bright (sort of) and early at 6:30 am yesterday (30th) morning before setting off at 7. The route took 4 and a half hours and, while it was chilly, we were really rather fortunate with the weather and we even got a sunny interval or two! We, unlike most of our fellow passengers, managed to remain on deck for the vast majority of the journey. There was of course good reason for this; we were amongst an iceberg dominated landscape across Disko Bay before approaching the island where mountains began to tower ahead.

We arrived into the harbour at Disko Island (known as Qeqertarsuaq in Greenlandic) at 11:30 and were picked up by Ole, the logistics manager at the University of Copenhagen’s Arktisk Station, where we shall be staying until the 9th August (except when we’re camping out in the field). The station is about a kilometre from the harbour and just outside the small town. Ole took us for tea in the library where we remained for some time and chatted about the station, the research project, and many other things.

After tea, we joined everyone for an amazing seafood buffet prepared for some very special visitors to the station. It was here that we were able to meet many of the other postgraduate researchers currently staying at the station. A short walk into town (via the puppies!) followed lunch and we bought some provisions for the days ahead. On returning to the station, we were shown our room by Arktisk Station’s manager, Akaaraq. The room is superb and has fantastic views out into Disko Bay where the icebergs slowly float by our window. In the evening, we went on a short walk around the town before returning station for some rest.

Today (the 31st), we have remained in the station where, after a small lie-in, we have spent much time preparing for the fieldwork and camping ahead. It’s just as well that our fieldwork is not starting today because the weather is somewhat wet and gloomy! Let’s hope that it improves for the days ahead.

Joe & Mark.

Looking back towards some icebergs just after leaving the port at Ilulissat A picture of me and Mark on the boat, taken by some American researchers who we met on the journey The approach to Disko Island (Qeqertarsuaq) A view of Arktisk Station from the beach. The town here on the island; the research station is on the far side from where this picture was taken, about a kilometre away.