Tropical lacustrine sediment microbial community response to an extreme El Niño event.

Salinity can influence microbial communities and related functional groups in lacustrine sediments, but few studies have examined temporal variability in salinity and associated changes in lacustrine microbial communities and functional groups. To better understand how microbial communities and functional groups respond to salinity, we examined geochemistry and functional gene amplicon sequence data collected from 13 lakes located in Kiritimati, Republic of Kiribati (2° N, 157° W) in July 2014 and June 2019, dates which bracket the very large El Niño event of 2015-2016 and a period of extremely high precipitation rates. Lake water salinity values in 2019 were significantly reduced and covaried with ecological distances between microbial samples.

Stable carbon isotope values of syndepositional carbonate spherules and micrite record spatial and temporal changes in photosynthesis intensity.

Marine and lacustrine carbonate minerals preserve carbon cycle information, and their stable carbon isotope values (δ C) are frequently used to infer and reconstruct paleoenvironmental changes. However, multiple processes can influence the δ C values of bulk carbonates, confounding the interpretation of these values in terms of conditions at the time of mineral precipitation. Co-existing carbonate forms may represent different environmental conditions, yet few studies have analyzed δ C values of syndepositional carbonate grains of varying morphologies to investigate their origins.

Human-induced ecological cascades: Extinction, restoration, and rewilding in the Galápagos highlands.

Oceanic islands support unique biotas but often lack ecological redundancy, so that the removal of a species can have a large effect on the ecosystem. The larger islands of the Galápagos Archipelago once had one or two species of giant tortoise that were the dominant herbivore. Using paleoecological techniques, we investigate the ecological cascade on highland ecosystems that resulted from whalers removing many thousands of tortoises from the lowlands.

Processing in Lateral Orbitofrontal Cortex Is Required to Estimate Subjective Preference during Initial, but Not Established, Economic Choice.

The orbitofrontal cortex (OFC) is proposed to be critical to economic decision making. Yet one can inactivate OFC without affecting well-practiced choices. One possible explanation of this lack of effect is that well-practiced decisions are codified into habits or configural-based policies not normally thought to require OFC.

Real-Time Value Integration during Economic Choice Is Regulated by Orbitofrontal Cortex.

Neural correlates implicate the orbitofrontal cortex (OFC) in value-based or economic decision making [1-3]. Yet inactivation of OFC in rats performing a rodent version of the standard economic choice task is without effect [4, 5], a finding more in accord with ideas that the OFC is primarily necessary for behavior when new information must be taken into account [6-9]. Neural activity in the OFC spontaneously updates to reflect new information, particularly about outcomes [10-16], and the OFC is necessary for adjustments to learned behavior only under these conditions [4, 16-26].

Medial orbitofrontal inactivation does not affect economic choice.

How are decisions made between different goods? One theory spanning several fields of neuroscience proposes that their values are distilled to a single common neural currency, the calculation of which allows for rational decisions. The orbitofrontal cortex (OFC) is thought to play a critical role in this process, based on the presence of neural correlates of economic value in lateral OFC in monkeys and medial OFC in humans. We previously inactivated lateral OFC in rats without affecting economic choice behavior.

Brief, But Not Prolonged, Pauses in the Firing of Midbrain Dopamine Neurons Are Sufficient to Produce a Conditioned Inhibitor.

Prediction errors are critical for associative learning. In the brain, these errors are thought to be signaled, in part, by midbrain dopamine neurons. However, although there is substantial direct evidence that brief increases in the firing of these neurons can mimic positive prediction errors, there is less evidence that brief pauses mimic negative errors.

Lateral Orbitofrontal Inactivation Dissociates Devaluation-Sensitive Behavior and Economic Choice.

How do we choose between goods that have different subjective values, like apples and oranges? Neuroeconomics proposes that this is done by reducing complex goods to a single unitary value to allow comparison. This value is computed "on the fly" from the underlying model of the goods space, allowing decisions to meet current needs. This is termed "model-based" behavior to distinguish it from pre-determined, habitual, or "model-free" behavior.

Spatiotemporal variability in the δO-salinity relationship of seawater across the tropical Pacific Ocean.

The relationship between salinity and the stable oxygen isotope ratio of seawater (δO) is of utmost importance to the quantitative reconstruction of past changes in salinity from δO values of marine carbonates. This relationship is often considered to be uniform across water masses, but the constancy of the δO-salinity relationship across space and time remains uncertain, as δO responds to varying atmospheric vapor sources and pathways, while salinity does not. Here we present new δO-salinity data from sites spanning the tropical Pacific Ocean.

Varied response of western Pacific hydrology to climate forcings over the last glacial period.

Atmospheric deep convection in the west Pacific plays a key role in the global heat and moisture budgets, yet its response to orbital and abrupt climate change events is poorly resolved. Here, we present four absolutely dated, overlapping stalagmite oxygen isotopic records from northern Borneo that span most of the last glacial cycle. The records suggest that northern Borneo's hydroclimate shifted in phase with precessional forcing but was only weakly affected by glacial-interglacial changes in global climate boundary conditions.

Impacts of climate variability and human colonization on the vegetation of the Galápagos Islands.

A high-resolution (2-9 year sampling interval) fossil pollen record from the Galápagos Islands, which spans the last 2690 years, reveals considerable ecosystem stability. Vegetation changes associated with independently derived histories of El Niño Southern Oscillation variability provided evidence of shifts in the relative abundance of individual species rather than immigration or extinction. Droughts associated with the Medieval Climate Anomaly induced rapid ecological change that was followed by a reversion to the previous state.