Climate impact of late quaternary equatorial pacific sea surface temperature variations

By D. Lea, D. Pak, Howard J. Spero. Science, 2000

1,069 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/837e392e75eac111c4021eb752afb65371db3945

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. R. Nigam
2. D. K. Naik
3. R. Saraswat
4. Andreas Mackensen
5. A. Clement
6. A. Broccoli
7. A. Hall
8. D. Lea

In Ecology

1. A. Clement
2. A. Broccoli
3. A. Hall
4. K. Carpenter
5. T. Harrison
6. D. Lea
7. A. Ridgwell
8. V. G. Springer

In Environmental Chemistry

1. R. Nigam
2. D. K. Naik
3. R. Saraswat
4. Andreas Mackensen
5. A. Clement
6. A. Hall
7. A. Broccoli
8. D. Lea

Citations in the corpus

• Primate Biogeography and Ecology on the Sunda Shelf Islands: A Paleontological and Zooarchaeological Perspective (2006, background): “In particular, oxygen isotope data confirm cooler seas during glacials and interstadials, and suggest that tropical seas were ∼5–6◦C cooler than today (e.g., Rind and Peteet, 1985; Chappell, 1994; Stute et al., 1995; Broecker, 1996; Bush and Philander, 1998; McCulloch et al., 1999; Lea et al., 2000)”
• The importance of precessional signals in the tropical climate (2004, methodology): “With new techniques in generating oceanic proxies of salinity change (e.g., Lea et al. 2000), it will be possible to unravel these hydrologic signals over the ocean, which are a fundamental part of the tropical climate response to external forcing.”
• El Niño–Southern Oscillation–like variability during glacial terminations and interlatitudinal teleconnections (2008, result): “SSTs lead d(18)O changes by 1 to 3 ka during glacial terminations, also in agreement with records from the EEP [Lea et al., 2000]”
• High-precision timeline for Earth’s most severe extinction (2014, result): “Using the maximum extinction duration of ∼60 ka, this suggests an ∼1 °C increase per 6,000 y, comparable to the rate and magnitude of the increase at the Paleocene–Eocene Thermal Maximum (PETM) (36) and Pleistocene/Holocene postglacial warming (∼2 °C/5 ka) (37).”
• Calcium isotopic composition of high-latitude proxy carrier Neogloboquadrina pachyderma (sin.) (2007, background): “7 E) based on Mg/Ca ratios in foraminifera (Lea et al., 2000) rendering strong support for a preserved temperature signal in theG.”
• Mid-Pleistocene revolution and the ‘eccentricity myth’ (2005, background): “Glacial periods are by their very nature drier which reduces atmospheric water vapour, and Lea et al. (2000) provide clear evidence that water vapour production of the equatorial Pacific zone was greatly curtailed during the last five glacial periods.”
• The center of the center of marine shore fish biodiversity: the Philippine Islands (2005, background): “However, both the Philippines and Wallacea are in the warmest region of the oceans, the western Pacific warm pool, which would have undergone approximately 3 C decrease during the last glacial maximum (Lea et al. 2000).”
• Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections (2013, methodology): “The Mg/Ca-based Malabar record indicates a slightly larger SST change; the observed change is, however, comparable with the 2.8 ± 0.7 °C change recorded for the equatorial Pacific (Lea et al., 2000) and other tropical Indian Ocean records (Saher et al., 2007a; Anand et al., 2008; Govil and Naidu, 20”