Climate reconstructing; it sounds elusive. Climate, that’s
weather averaged out over a period of 30 years. But weather is so evanescent!
The wind, sunshine, rainfall we experience one day; how much is left of that
the next day? Let alone 30 years later. Climate
reconstruction therefore has to rely on indirect measures. You want to know how
windy it was at a given place, over a period of time? Find a place where
wind-blown dust would accumulate, and measure its grain size through time. It evidently
takes stronger winds to transport larger grains. And you have to be careful
that you’re not looking at a record of dust availability, but if you’ve ruled
that out, you may have managed to reconstruct
the elusive wind. Trying to reconstruct sunlight? You might manage to
find pollen of various species of plants; some that need more sunlight than
others. Rainfall? Try to find a dripstone cave; the stalagmites in it are
likely to have recorded that in their isotopic signature.
One of the big and attention-grabbing factors of modern
climate change is sea ice. It is vanishing rapidly from the Northern hemisphere (see, for instance, here),
and, due to its reflective properties, that is not something that can or should
go unnoticed (see, for instance, here). But if
you want to understand it, and thus try to reconstruct its behaviour in the
past; how would you grasp that? If it melts it’s gone. But it’s not more gone
that the sunshine or the rain. Of course we have ways…
Thick sea ice
Big icebergs that have calved from a glacier are easy to
trace. During their time as a part of the glacier, they pick up material of all
kinds – from clay to boulders. And while they melt, they deposit that on the
sea floor as so-called ice rafted debris. An iceberg will
float into the open sea, where rivers can’t reach, rather soon, so if you find
coarse sediment in a region like that, you know who the culprit must have been.
But these icebergs are not the big player in the climate system; that’s the sea
ice that froze straight from the sea water. That covers the big expanses of the
polar oceans, and reflects all of that light back into space. How to get a
handle on that?
Quite a lot of sea ice is so thick it doesn’t let any
sunlight through. This means that not much can live in the sea water
underneath. Any nutrients below sea ice will just float around, uneaten. But
when they reach the edge of the ice, all the photosynthesizers will pounce on that
opulence. The ice edge is often the most biologically vibrant part of a polar
sea. And quite often, the ice edge will be where two water masses meet: an
incoming warm current will stop ice advance in its way, and the mixing waters
will makes the situation even more dynamic. Early on, researchers realised
that, and figured that if you just trace the movings around of the high
densities of marine microorganisms who like fresh food you are likely tracing
the ice edge. But these organisms are not always very well preserved. And even
if they are; it is a somewhat indirect measure. There may well be other reasons
there is high productivity somewhere. Before you know it, you are tracing a
plume of nutritious wind-blown dust…
Nonionellina labradorica; a foraminifer often found near the ice edge
Later on, people figured out that something quite relevant
lives attached to the (thinner) sea ice: sea ice algae. And they contain
biological compound, which they called IP25, and which is not found
anywhere else, and which is very resistant to degradation. Find this in your
sediment, and know for sure there has been sea ice overhead. This kicked sea
ice reconstruction into a higher gear. Never before had something measurable in
sediment been so unequivocally linked to the presence of sea ice! Drill a
transect of cores, date them, measure this organic compound through the cores
and you know how far the ice has reached over the time period covered by the
sediments in your core (provided you chose your transect wisely). So have we
finally found a method of environmental reconstruction without caveats? Well
no, of course not. First of all, if you don’t find this compound it doesn’t
necessarily mean there was no sea ice; it might just have been so thick it
didn’t let any light through, so the algae couldn’t live under it. And another
issue is: when do you consider an area of sea covered by ice? If it’s entirely
covered? When it’s mostly covered? What are you really reconstructing when you
find this IP25?
Sea ice algae. Source: NOAA
Fortunately, there are people who will just tirelessly run
marine sediments through mass spectrometers, always looking for more chemical
compounds that might be indicative of something interesting. And some found a
set of additional biomarkers associated only with open water. That allowed us
first to distinguish between the absence of IP25 due to absence of ice, and due
to overbearing presence of ice. And, helped by calibration with satellite
imagery, other workers later even managed to use both components to quantify
how much of the water had been covered by ice during the growth of the algae
that had produced the IP25. This means we now have ways of getting a handle on
where there has been how much sea ice over long periods of time, which would
hardly have been dreamed of during the turn of the century. So it takes 21th
century organic geochemistry to know when there has been how much sea ice at a
given location. But in the end, you’re just asking some algae…
Partial sea-ice cover
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