Numerous temperature and environmental proxies are based on glycerol dialkyl glycerol tetraethers (GDGTs), which are membrane lipids commonly found in the water columns and sediments of lakes. The TEX86 temperature proxy is based on isoprenoid GDGTs, which are produced by members of the archaea, and is used to reconstruct lake surface temperature. Branched GDGTs are lipids produced by bacteria and form the basis of the MBT′5ME temperature proxy. Although many outstanding questions still exist regarding proxies based on isoprenoid and branched GDGTs, both compound classes have been relatively well-studied in lakes. More recently, other types of GDGTs and related compounds are increasingly being reported from lacustrine sediments including hydroxylated GDGTs (OH-GDGTs) and glycerol monoalkyl glycerol tetraethers (GMGTs). In the process of generating lacustrine TEX86 or MBT′5ME temperature records, we noted that OH-GDGTs or GMGTs (or both) are frequently present. The RI-OH, based on OH-GDGTs, recently has been proposed as a temperature proxy in lakes while GMGTs are associated with oxygen-deficient environments. Here we examine distributions of OH-GDGTs and GMGTs in a variety of lakes that also have existing TEX86 or MBT’5ME temperature reconstructions. These lakes range from small to large, shallow to deep, tropical to arctic, differ in oxygenation state, and have sedimentary records covering timespans from the Holocene to multiple glacial-interglacial cycles. Study lakes include El’gygytgyn (arctic Russia), Malawi (tropical southeast Africa), Issyk Kul (Kyrgyzstan), Lake 578 (Greenland), and high elevation lakes in the central Andes (South America). We explore the presence/absence of these compounds in contrasting depositional environments and examine their GDGT distributions in relationship to temperature variability, oxic/anoxic conditions, hydroclimate fluctuations, and other geochemical/environmental parameters.
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Biomarker characterization of the North Water Polynya, Baffin Bay: implications for local sea ice and temperature proxies
Abstract. The North Water Polynya (NOW, Inuktitut: Sarvarjuaq; Kalaallisut:Pikialasorsuaq), Baffin Bay, is the largest polynya and one of the most productive regionsin the Arctic. This area of thin to absent sea ice is a critical moisturesource for local ice sheet sustenance and, coupled with the inflow ofnutrient-rich Arctic Surface Water, supports a diverse community of Arcticfauna and indigenous people. Although paleoceanographic records provideimportant insight into the NOW's past behavior, it is critical that webetter understand the modern functionality of paleoceanographic proxies. Inthis study, we analyzed lipid biomarkers, including algal highly branchedisoprenoids and sterols for sea ice extent and pelagic productivity andarchaeal glycerol dibiphytanyl glycerol tetraethers (GDGTs) for ocean temperature, in a set of modern surface sedimentsamples from within and around the NOW. In conjunction with previouslypublished datasets, our results show that all highly branched isoprenoidsexhibit strong correlations with each other and not with sterols, whichsuggests a spring or autumn sea ice diatom source for all highly branched isoprenoids (HBIs) rather than acombination of sea ice and open-water diatoms as seen elsewhere in theArctic. Sterols are also highly concentrated in the NOW and exhibitstatistically higher concentrations here compared to sites south of the NOW,consistent with the order of magnitude higher primary productivity observedwithin the NOW relative to surrounding waters in spring and summer months.Finally, our local temperature calibrations for GDGTs and OH-GDGTs reducethe uncertainty present in global temperature calibrations but alsoidentify some additional variables that may be important in controllingtheir local distribution, such as nitrate availability and dissolved oxygen.Collectively, our analyses provide new insight into the utility of theselipid biomarker proxies in high-latitude settings and will help provide arefined perspective on the past development of the NOW with theirapplication in downcore reconstructions.
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- Award ID(s):
- 1804504
- PAR ID:
- 10561641
- Publisher / Repository:
- AGU
- Date Published:
- Journal Name:
- Biogeosciences
- Volume:
- 20
- Issue:
- 1
- ISSN:
- 1726-4189
- Page Range / eLocation ID:
- 229 to 249
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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