Clathromorphum (a calcified ALGA!) meets requirements for climate archive
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- George Casey
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1 Clathromorphum (a calcified ALGA!) meets requirements for climate archive Exhibit high temporal climate recording resolution Multicentury-scale lifespan Abundant in Arctic and Subarctic Accurately records climate information?
2 Crustose coralline algal-based marine climate reconstructions 1. Bering Sea teleconnections 2. Crusty algae uncover sea-ice change 3. Coralline algae and ocean acidification
3 Arctic Bering Sea Attu Subarctic North Pacific
4 Clathromorphum nereostratum, Aleutian Islands Laterally continuous growth increments No apparent growth interruptions Life span ca. 151 years (based on annual growth increment counting) 1969 collected live in cm
5 How can we measure Mg/Ca ratio? Electron microprobe Electron beam spot size 5 m 15 samples/year on average Hetzinger et al. 2009
6 Sea Surface Temperature ( C) Mg/Ca ratios Temperature indicator Mg/Ca ratio Temperature ( C) Hetzinger, Halfar et al. 2011, PPP
7 Algal Mg/Ca record Hetzinger, Halfar et al. 2012, Climate Dynamics
8 Comparison of Mg/Ca and regional sea surface temperatures Hetzinger, Halfar et al. 2012, Climate Dynamics
9 Interbasin comparison: Bering Sea-Atlantic Teleconnection (Teleconnection: Climate anomalies related to each other at large distances) Modeling studies have speculated on interbasin linkage Investigations hampered by limited length of reliable instrumental data Algal time series is first 150-year temperature record from Bering Sea Teleconnection
10 Background Bering Sea Teleconnections Labrador Sea Variability Ocean Acidification Arctic Interbasin comparison: Bering Sea-Atlantic Teleconnections Aleutian Mg/Ca Record - North Atlantic Oscillation NAO: - Mode of natural climate variability in North Atlantic - Atmospheric pressure difference Icelandic Low and Azores High
11 Background Bering Sea Teleconnections Labrador Sea Variability Ocean Acidification Arctic Interbasin comparison: Bering Sea-Atlantic Teleconnections Aleutian Mg/Ca Record - North Atlantic Oscillation NAO: - Mode of natural climate variability in North Atlantic - Atmospheric pressure difference Icelandic Low and Azores High - Controls strength of westerlies + storm tracks across North Atlantic Large pressure difference (positive NAO) results in increased westerlies mild and wet winters in Central Europe
12 Interbasin comparison: Bering Sea-Atlantic Teleconnections Aleutian Mg/Ca Record - North Atlantic Oscillation Hetzinger, Halfar et al. 2012, Climate Dynamics
13 Multisample Mg/Ca record from Bering Sea n=6 Williams et al., in prep.
14 * * * * * * * * * **
15 Crusty algae uncover sea-ice change
16 Sea-ice extent is declining faster than models predict! Improve models by calibrating them with long time series of past sea ice extent Jeffries et al. 2013
17 Present knowledge about past sea ice distribution: Satellite data (since 1979) Observational information (sparse before ~1850)
18 Present knowledge about past sea ice distribution: Satellite data (since 1979) Observational information (sparse before ~1920) Sea Ice Proxies -Low-resolution marine sediment cores -Remote terrestrial archives Ice cores Need to search for high-resolution in situ marine sea-ice recorder
19 Characteristics of Clathromorphum Photosynthetic calcifier Can live under sea ice
20 Characteristics of Clathromorphum Photosynthetic calcifier Can live under sea ice
21 Growth Rates function of Light and Temperature 0.29 mm 0.20 mm 0.18 mm 0.16 mm 0.24 mm 0.26 mm 0.28 mm 0.21 mm mm
22 Sea-Ice Loss Past Sea Ice Coralline Archives Corallines and Sea Ice 650-year Record Growth rates Indicator of length of ice cover + summer temperature Seasonal Ice Cover * Arctic Bay * * * * Gulf of Maine From Adey, Halfar, Williams 2013
23 Mg/Ca ratios Temperature indicator + length of summer growth season
24 Combination of Growth rates Indicator of length of ice cover + summer temperature and Mg/Ca ratios Indicator of temperatures + length of summer growth season Ice cover proxy
25 * *
26 * *
27 Correlation to Satellite Data Halfar et al. 2013, PNAS
28 Relationship to Historical Data and Climate Halfar et al. 2013
29 Longest continuous time series from live-collected coralline alga Onset of Little Ice Age coincides with expansion of Inuit 20 th century sea-ice decline in NW Atlantic unprecedented in last 650 years Halfar et al. 2013
30 Halfar et al. 2013
31 Halfar et al. 2013
32 Coralline Bering algae Sea Teleconnections High-resolution environmental Sea archives Ice Change - Sea-ice reconstructions Ocean Acidification Halfar et al. 2013
33 Interannual frequency dominates during cold intervals such as the LIA Multidecadal frequency dominates during warm intervals Halfar et al. 2013
34 Coralline algae and Ocean acidification
35 CO 2 Since 1700 Hoegh-Guldberg et al. 2007
36 Are Clathromorphum carbonates susceptible to ocean acidification? Aragonitic corals may already show decrease in calcification rates Year From De ath et al 2009
37 Our question: Do cold water coralline algae (High Mg-Calcite) show a similar decline? Answer:
38 Ocean Carbon Chemistry Carbonate Minerals CaCO 3 + CO 2 + H 2 O Ca HCO 3 - Calcite Aragonite Mg-Calcite Ikaite + Magnesium Increasing Solubility
39 Saturation State Bering Sea Teleconnections Sea Ice Change Ocean Acidification Andersson et al Geology High Mg-calcites exceed solubility of aragonite at ~12 mol% MgCO 3 Cold-water coralline algae have up to 18 mol% MgCO 3
40 Aragonite Saturation (~Mg-Calcite 12 mol%mgco 3 ) Aragonite Saturation ( mol kg -1 ) * from Orr et al 2005
41 Aragonite Saturation (~Mg-Calcite 12 mol%mgco 3 ) Aragonite Saturation ( mol kg -1 ) from Orr et al 2005
42 Calcification Rate (g/cm 3 /yr) = Growth rate x Skeletal Density
43 Calcification Rate (g/cm 3 /yr) = Growth rate x Skeletal Density 0.29 mm 0.20 mm 0.18 mm 0.16 mm 0.24 mm 0.26 mm 0.28 mm 0.21 mm mm
44 Calcification Rate (g/cm 3 /yr) = Growth rate x Skeletal Density Micro Computer Tomography Resolution 20 microns Series of two-dimensional x-ray images Imaging + quantitative measurement of skeletal density 1 mm
45 Bering Sea Teleconnections Sea Ice Change Ocean Acidification Young 1 mm Old
46 n=8 Chan, Halfar et al. subm.
47 n=8 Chan, Halfar et al. subm.
48 n=8 Chan, Halfar et al. subm.
49 n=8 Chan, Halfar et al. subm.
50 Clathromorphum buildups resilient to present-day effects of ocean acidification Resilience possibly due to metabolic control over calcification Until what ph can metabolic control be maintained? Present Future?
51 Questions? RV Alca i
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