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. Author manuscript; available in PMC: 2013 Nov 1.
Published in final edited form as: Environ Res. 2012 May 8;119:27–41. doi: 10.1016/j.envres.2012.03.011

Table 4.

Mercury concentrations in sediments (ng g−1 dry weight) of the major physioregions of the Gulf of Maine.

Description Total Hg MeHg Year(s) Reference
Bay of Fundy
Passamaquoddy Bay
Bay of Fundy mouth
Intertidal marshes

Bay of Fundy wide
42±13
16±6.2
7–79

30 (20–90)
0.30±0.09
0.10±0.02
2000–2002

1997–2002

1977
Sunderland et al. (2004; 2006)
(Hung and Chmura, 2006)


Loring (1982)
Eastern Coastal Shelf No data No data - -
Northern Coastal Shelf
Penobscot Rivera

Penobscot River estuary
  Upper estuary
  Lower estuary
Mount Desert Island, ME
Wells, ME
Casco Bay, ME
Great Bay estuary, NH:
Mudflats
Coastal salt marsh
200–86,200


200–1,450
20–140
8.5–9.0
8–83
n/d – 490

40–1420
43–440
0.1–74.2


7.5–20
0.2–1.7
0.37
0.15–0.59


0.08–3.88
0.04–2.20
1998–2000

2006–2007


2006–2007
2006–2007
2000–2001

2008–2010
(Camp Dresser & McKee Inc., 2001)
Bodaly et al. (2008)



Chen et al. unpublished data
Wade et al. (2008)
Amirbahman et al. unpublished data
Southern Coastal Shelf
Boston Harbor 501–2200

250–1000
1.0–9.0 2003

1993
Benoit et al. (2006; 2009)

Bothner et al. (1998)
Offshore Regionsb n/d-20 No data 1990s (Buchholtz ten Brink et al., 2002)

n/d = below detection limits.

a

The Penobscot River received large amounts of industrial Hg contamination from several pulp and paper mills and a chlor-alkali facility that closed in 2000.

b

Includes Brown’s Bank, Central Gulf of Maine, Georges Bank, Great South Channel, Georges Channel, Jordan Basin, and Wilkinson Basin.