The science team measured many properties using various
instruments and microscopic observations and we are still processing the main
findings. The scientists are trained in many different disciplines, from biology to chemistry to physics, because geology (or geoscience) is an interdisciplinary science. A few examples of types of shipboard measurements and observations are described below.
Lithologies (sand or mud) and sedimentary structures: like the cross-sections of
ripples in the sand on a beach, but here encased in deep-sea mud. The ripple structures tell us something about variations in how
fast the deep ocean currents were flowing. These currents are wind-driven or gravity driven (like rivers), so
indirectly they let us know how strong the winds were in the past or how much material was coming down from the continent in deep-sea channels.
Cobbles and pebbles:
the rocks are full of mineral crystals that point to a type of
volcanic process. Some of these rocks are unique to specific locations in West
Antarctica. The rocks were taken up by the glacial ice and transported offshore
as icebergs broke off from the land ice. Hence these rocks tell us about the
locations on West Antarctica where ice was released into the ocean by the
calving of glaciers in the past.
Physical properties: for example, how fast sound waves travel through a rock core is determined by how dense and springy the material is. Sound waves travel fast in hard, cemented, layers (see also below). The natural radio-activity of the cores is another physical property that is measured. The natural radio-activity is lower when more fossil material is present, which is not as naturally radioactive as material brought in from land. In the Antarctic ocean, we can use the natural radio-activity of core sections together with microscopic observations of fossil marine algae to estimate how often open ocean without sea ice was present through time.
Pore water chemistry: water within the rock was squeezed out (see squeezers to the right) and analyzed chemically to understand how sediments and water change down to hundreds of meters
beneath the seafloor. For example, we found layers of sand grains that were
cemented together into a hard rock, like concrete. The compounds that make up
the cement typically come from the pore waters. To tie all these different measurements together, we have had integrated meetings with all the 30 or so scientists on board.
In the next few years we will be able to write the history
book of the West Antarctic Ice Sheet and how it developed through past warm
periods using the shipboard data and additional measurements in shore-based
labs. We will be able to place the present accelerating melt of the floating
glacial ice in the Amundsen Sea embayment into a long-term framework of many
generations and in the process educate the scientists of the future!
The ship is now made ready for Expedition 382 Iceberg Alley, another Antarctic expedition with the JOIDES Resolution drillship. Our shipboard crew and science party will leave the ship on Wednesday and a whole new crew and science party will get on board. If you are interested in following the Iceberg Alley expedition, make sure you follow @jr on Twitter and blogs could be available at joidesresolution.org.
