<p><strong>Abstract.</strong> Large-scale magmatic events like the emplacement of the North Atlantic
Igneous Province (NAIP) are often coincident with periods of extreme climate
change such as the Palaeocene–Eocene Thermal Maximum (PETM). One proxy for
volcanism in the geological record that is receiving increased attention is
the use of mercury (Hg) anomalies. Volcanic eruptions are among the dominant
natural sources of Hg to the environment; thus, elevated <span class="inline-formula">Hg∕TOC</span> values
in the sedimentary rock record may reflect an increase in volcanic activity
at the time of deposition. Here we focus on five continental shelf sections
located around the NAIP in the Palaeogene. We measured Hg concentrations,
total organic carbon (TOC) contents, and <span class="inline-formula"><i>δ</i><sup>13</sup>C</span> values to assess
how Hg deposition fluctuated across the PETM carbon isotope excursion (CIE).
We find a huge variation in Hg anomalies between sites. The Grane field in
the North Sea, the most proximal locality to the NAIP analysed, shows Hg
concentrations up to 90 100 ppb
(<span class="inline-formula">Hg∕TOC</span> <span class="inline-formula">=</span> 95 700 ppb wt %<span class="inline-formula"><sup>−1</sup></span>) in the early Eocene.
Significant <span class="inline-formula">Hg∕TOC</span> anomalies are also present in Danish (up to
324 ppb wt %<span class="inline-formula"><sup>−1</sup></span>) and Svalbard (up to 257 ppb wt %<span class="inline-formula"><sup>−1</sup></span>)
sections prior to the onset of the PETM and during the recovery period, while
the Svalbard section also shows a continuous <span class="inline-formula">Hg∕TOC</span> anomaly during the
body of the CIE. The combination with other tracers of volcanism, such as tephra
layers and unradiogenic Os isotopes, at these localities suggests that the
<span class="inline-formula">Hg∕TOC</span> anomalies reflect pulses of magmatic activity. In contrast, we
do not observe clear Hg anomalies on the New Jersey shelf (Bass River) or the
Arctic Ocean (Lomonosov Ridge). This large spatial variance could be due to
more regional Hg deposition. One possibility is that phreatomagmatic
eruptions and hydrothermal vent complexes formed during the emplacement of
sills led to submarine Hg release, which is observed to result in limited
distribution in the modern era. The <span class="inline-formula">Hg∕TOC</span> anomalies in strata
deposited prior to the CIE may suggest that magmatism linked to the
emplacement of the NAIP contributed to the initiation of the PETM. However,
evidence for considerable volcanism in the form of numerous tephra layers and
<span class="inline-formula">Hg∕TOC</span> anomalies post-PETM indicates a complicated relationship
between LIP volcanism and climate. Factors such as climate system feedbacks,
changes to the NAIP emplacement style, and/or varying magma production rates
may be key to both the onset and cessation of hyperthermal conditions during
the PETM. However, processes such as<span id="page218"/> diagenesis and organic matter sourcing
can have a marked impact on <span class="inline-formula">Hg∕TOC</span> ratios and need to be better
constrained before the relationship between Hg anomalies and volcanic
activity can be considered irrefutable.</p>
